Articles | Volume 15, issue 12
https://doi.org/10.5194/se-15-1525-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-15-1525-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
20 Dec 2024
Research article |
| 20 Dec 2024
| 20 Dec 2024
Reconciling post-orogenic faulting, paleostress evolution, and structural inheritance in the seismogenic northern Apennines (Italy): insights from the Monti Martani Fault System
University of Bologna – Department of Biological, Geological and Environmental Sciences (BIGEA), Bologna, Italy
Selina Bonini
University of Bologna – Department of Biological, Geological and Environmental Sciences (BIGEA), Bologna, Italy
Giulio Viola
University of Bologna – Department of Biological, Geological and Environmental Sciences (BIGEA), Bologna, Italy
Gianluca Vignaroli
University of Bologna – Department of Biological, Geological and Environmental Sciences (BIGEA), Bologna, Italy
Related authors
Selina Bonini, Riccardo Asti, Giulio Viola, Giulia Tartaglia, Stefano Rodani, Gianluca Benedetti, Massimo Comedini, and Gianluca Vignaroli
EGUsphere, https://doi.org/10.5194/egusphere-2025-506, https://doi.org/10.5194/egusphere-2025-506, 2025
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Considering the structural complexity related to the internal architecture of active and capable faults, seismic hazard may be linked to different fault attributes depending on the fault domain crossed by a linear infrastructure. We propose a structural geology-based approach for the preliminary study of the area potentially affected by earthquake-induced surface ruptures during infrastructural design, based on the geometric relationships between the active fault and the infrastructure itself.
Paul Angrand, Frédéric Mouthereau, Emmanuel Masini, and Riccardo Asti
Solid Earth, 11, 1313–1332, https://doi.org/10.5194/se-11-1313-2020, https://doi.org/10.5194/se-11-1313-2020, 2020
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We study the Iberian plate motion, from the late Permian to middle Cretaceous. During this time interval, two oceanic systems opened. Geological evidence shows that the Iberian domain preserved the propagation of these two rift systems well. We use geological evidence and pre-existing kinematic models to propose a coherent kinematic model of Iberia that considers both the Neotethyan and Atlantic evolutions. Our model shows that the Europe–Iberia plate boundary was made of two rift systems.
Selina Bonini, Riccardo Asti, Giulio Viola, Giulia Tartaglia, Stefano Rodani, Gianluca Benedetti, Massimo Comedini, and Gianluca Vignaroli
EGUsphere, https://doi.org/10.5194/egusphere-2025-506, https://doi.org/10.5194/egusphere-2025-506, 2025
Short summary
Short summary
Considering the structural complexity related to the internal architecture of active and capable faults, seismic hazard may be linked to different fault attributes depending on the fault domain crossed by a linear infrastructure. We propose a structural geology-based approach for the preliminary study of the area potentially affected by earthquake-induced surface ruptures during infrastructural design, based on the geometric relationships between the active fault and the infrastructure itself.
Matthew S. Hodge, Guri Venvik, Jochen Knies, Roelant van der Lelij, Jasmin Schönenberger, Øystein Nordgulen, Marco Brönner, Aziz Nasuti, and Giulio Viola
Solid Earth, 15, 589–615, https://doi.org/10.5194/se-15-589-2024, https://doi.org/10.5194/se-15-589-2024, 2024
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Smøla island, in the mid-Norwegian margin, has complex fracture and fault patterns resulting from tectonic activity. This study uses a multiple-method approach to unravel Smøla's tectonic history. We found five different phases of deformation related to various fracture geometries and minerals dating back hundreds of millions of years. 3D models of these features visualise these structures in space. This approach may help us to understand offshore oil and gas reservoirs hosted in the basement.
Alberto Ceccato, Giulia Tartaglia, Marco Antonellini, and Giulio Viola
Solid Earth, 13, 1431–1453, https://doi.org/10.5194/se-13-1431-2022, https://doi.org/10.5194/se-13-1431-2022, 2022
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The Earth's surface is commonly characterized by the occurrence of fractures, which can be mapped, and their can be geometry quantified on digital representations of the surface at different scales of observation. Here we present a series of analytical and statistical tools, which can aid the quantification of fracture spatial distribution at different scales. In doing so, we can improve our understanding of how fracture geometry and geology affect fluid flow within the fractured Earth crust.
Giulio Viola, Giovanni Musumeci, Francesco Mazzarini, Lorenzo Tavazzani, Manuel Curzi, Espen Torgersen, Roelant van der Lelij, and Luca Aldega
Solid Earth, 13, 1327–1351, https://doi.org/10.5194/se-13-1327-2022, https://doi.org/10.5194/se-13-1327-2022, 2022
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A structural-geochronological approach helps to unravel the Zuccale Fault's architecture. By mapping its internal structure and dating some of its fault rocks, we constrained a deformation history lasting 20 Myr starting at ca. 22 Ma. Such long activity is recorded by now tightly juxtaposed brittle structural facies, i.e. different types of fault rocks. Our results also have implications on the regional evolution of the northern Apennines, of which the Zuccale Fault is an important structure.
Leonardo Del Sole, Marco Antonellini, Roger Soliva, Gregory Ballas, Fabrizio Balsamo, and Giulio Viola
Solid Earth, 11, 2169–2195, https://doi.org/10.5194/se-11-2169-2020, https://doi.org/10.5194/se-11-2169-2020, 2020
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This study focuses on the impact of deformation bands on fluid flow and diagenesis in porous sandstones in two different case studies (northern Apennines, Italy; Provence, France) by combining a variety of multiscalar mapping techniques, detailed field and microstructural observations, and stable isotope analysis. We show that deformation bands buffer and compartmentalize fluid flow and foster and localize diagenesis, recorded by carbonate cement nodules spatially associated with the bands.
Paul Angrand, Frédéric Mouthereau, Emmanuel Masini, and Riccardo Asti
Solid Earth, 11, 1313–1332, https://doi.org/10.5194/se-11-1313-2020, https://doi.org/10.5194/se-11-1313-2020, 2020
Short summary
Short summary
We study the Iberian plate motion, from the late Permian to middle Cretaceous. During this time interval, two oceanic systems opened. Geological evidence shows that the Iberian domain preserved the propagation of these two rift systems well. We use geological evidence and pre-existing kinematic models to propose a coherent kinematic model of Iberia that considers both the Neotethyan and Atlantic evolutions. Our model shows that the Europe–Iberia plate boundary was made of two rift systems.
Francesca Prando, Luca Menegon, Mark Anderson, Barbara Marchesini, Jussi Mattila, and Giulio Viola
Solid Earth, 11, 489–511, https://doi.org/10.5194/se-11-489-2020, https://doi.org/10.5194/se-11-489-2020, 2020
Barbara Marchesini, Paolo Stefano Garofalo, Luca Menegon, Jussi Mattila, and Giulio Viola
Solid Earth, 10, 809–838, https://doi.org/10.5194/se-10-809-2019, https://doi.org/10.5194/se-10-809-2019, 2019
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We documented the role of fluids in the initial embrittlement of the Svecofennian basement and subsequent strain localization and fault evolution at the brittle–ductile transition zone. We studied the fault rocks of a deeply exhumed fault system characterized by mixed brittle–ductile deformation. Results from fluid inclusions, mineral chemistry, and geothermometry of synkinematic minerals document the ingress of distinct fluid batches and fluid pressure oscillations.
Mirko Carlini, Giulio Viola, Jussi Mattila, and Luca Castellucci
Solid Earth, 10, 343–356, https://doi.org/10.5194/se-10-343-2019, https://doi.org/10.5194/se-10-343-2019, 2019
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Physical properties of layered sedimentary rocks affect nucleation and propagation of discontinuities therein. Fractures developing through sedimentary sequences characterized by the alternation of strong and weak layers are strongly deviated along their track at layers’ boundaries, and depending on the layer they cross-cut, they show very thick (strong layers) or very thin (weak layers) infills of precipitated minerals, potentially representing pathways for ore deposits and oil/water resources.
Related subject area
Subject area: Tectonic plate interactions, magma genesis, and lithosphere deformation at all scales | Editorial team: Structural geology and tectonics, paleoseismology, rock physics, experimental deformation | Discipline: Structural geology
Poro–perm relations of Mesozoic carbonates and fault breccia, Araxos Promontory, NW Greece
The size distributions of fractures and earthquakes: implications for orogen-internal seismogenic deformation
Strike-slip kinematics from crustal to outcrop-scale: the impact of material properties on analogue modelling
Lithologically constrained velocity–density relationships and vertical stress gradients in the North Alpine Foreland Basin, SE Germany
Unbiased statistical length analysis of linear features: adapting survival analysis to geological applications
Earthquake swarms frozen in an exhumed hydrothermal system (Bolfin Fault Zone, Chile)
Computational modelling and analytical validation of singular geometric effects in fault data using a combinatorial algorithm
Dissolution-precipitation creep in polymineralic granitoid shear zones in experiments I: Strain localization mechanisms
Understanding the stress field at the lateral termination of a thrust fold using generic geomechanical models and clustering methods
Localized shear and distributed strain accumulation as competing shear accommodation mechanisms in crustal shear zones: constraining their dictating factors
Influence of water on crystallographic preferred orientation patterns in a naturally deformed quartzite
Geomorphic expressions of active rifting reflect the role of structural inheritance: a new model for the evolution of the Shanxi Rift, northern China
Driven magmatism and crustal thinning of coastal southern China in response to subduction
Selection and characterization of the target fault for fluid-induced activation and earthquake rupture experiments
Naturally fractured reservoir characterisation in heterogeneous sandstones: insight for uranium in situ recovery (Imouraren, Niger)
Multiscalar 3D temporal structural characterisation of Smøla island, mid-Norwegian passive margin: an analogue for unravelling the tectonic history of offshore basement highs
Impact of faults on the remote stress state
Subduction plate interface shear stress associated with rapid subduction at deep slow earthquake depths: example from the Sanbagawa belt, southwestern Japan
Multiple phase rifting and subsequent inversion in the West Netherlands Basin: implications for geothermal reservoir characterization
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Natural fracture patterns at Swift Reservoir anticline, NW Montana: the influence of structural position and lithology from multiple observation scales
Rapid hydration and weakening of anhydrite under stress: implications for natural hydration in the Earth's crust and mantle
Analogue experiments on releasing and restraining bends and their application to the study of the Barents Shear Margin
Structural framework and timing of the Pahtohavare Cu ± Au deposits, Kiruna mining district, Sweden
Does the syn- versus post-rift thickness ratio have an impact on the inversion-related structural style?
Inversion of accommodation zones in salt-bearing extensional systems: insights from analog modeling
Structural control of inherited salt structures during inversion of a domino basement-fault system from an analogue modelling approach
Kinematics and time-resolved evolution of the main thrust-sense shear zone in the Eo-Alpine orogenic wedge (the Vinschgau Shear Zone, eastern Alps)
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Time-dependent frictional properties of granular materials used in analogue modelling: implications for mimicking fault healing during reactivation and inversion
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Analogue modelling of the inversion of multiple extensional basins in foreland fold-and-thrust belts
A contribution to the quantification of crustal shortening and kinematics of deformation across the Western Andes ( ∼ 20–22° S)
Rift thermal inheritance in the SW Alps (France): insights from RSCM thermometry and 1D thermal numerical modelling
The Luangwa Rift Active Fault Database and fault reactivation along the southwestern branch of the East African Rift
Clustering has a meaning: optimization of angular similarity to detect 3D geometric anomalies in geological terrains
Shear zone evolution and the path of earthquake rupture
Mechanical compaction mechanisms in the input sediments of the Sumatra subduction complex – insights from microstructural analysis of cores from IODP Expedition 362
Detecting micro fractures: a comprehensive comparison of conventional and machine-learning-based segmentation methods
Multiscale lineament analysis and permeability heterogeneity of fractured crystalline basement blocks
Structural characterization and K–Ar illite dating of reactivated, complex and heterogeneous fault zones: lessons from the Zuccale Fault, Northern Apennines
How do differences in interpreting seismic images affect estimates of geological slip rates?
Progressive veining during peridotite carbonation: insights from listvenites in Hole BT1B, Samail ophiolite (Oman)
Tectonic evolution of the Indio Hills segment of the San Andreas fault in southern California, southwestern USA
Structural diagenesis in ultra-deep tight sandstones in the Kuqa Depression, Tarim Basin, China
Variscan structures and their control on latest to post-Variscan basin architecture: insights from the westernmost Bohemian Massif and southeastern Germany
Multi-disciplinary characterizations of the BedrettoLab – a new underground geoscience research facility
Biotite supports long-range diffusive transport in dissolution–precipitation creep in halite through small porosity fluctuations
Sergio C. Vinciguerra, Federico Vagnon, Irene Bottero, Jerome Fortin, Angela Vita Petrullo, Dimitrios Spanos, Aristotelis Pagoulatos, and Fabrizio Agosta
Solid Earth, 16, 681–707, https://doi.org/10.5194/se-16-681-2025, https://doi.org/10.5194/se-16-681-2025, 2025
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We assessed the poro–perm relations of both host rocks and fault rocks of Mesozoic carbonate rocks, by integrating a laboratory petrophysical study with a digital image analysis. Three different protocols were employed to compute permeability: (i) Effective Medium Theory on laboratory data, (ii) constant crack aperture and (iii) crack density values from 2D images. Carbonate host rocks did not show a clear poro–perm trend due to the presence of stiff, sub-rounded pores and of small vugs.
Sandro Truttmann, Tobias Diehl, Marco Herwegh, and Stefan Wiemer
Solid Earth, 16, 641–662, https://doi.org/10.5194/se-16-641-2025, https://doi.org/10.5194/se-16-641-2025, 2025
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Our study investigates the statistical relationship between geological fractures and earthquakes in the southwestern Swiss Alps. We analyze how the fracture size and earthquake rupture are related and find differences in how fractures at different depths rupture seismically. While shallow fractures tend to rupture only partially, deeper fractures are more likely to rupture along their entire length, potentially resulting in larger earthquakes.
Luigi Massaro, Jürgen Adam, Elham Jonade, Silvia Negrão, and Yasuhiro Yamada
Solid Earth, 16, 531–550, https://doi.org/10.5194/se-16-531-2025, https://doi.org/10.5194/se-16-531-2025, 2025
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In this manuscript, we investigated the kinematics and dynamics of strike-slip damage zones using laboratory mechanical tests and analogue modelling techniques. The results underline the importance of a multi-scale approach (from crustal to outcrop-scale) to improve the understanding of such deformation processes, deriving fundamental correlations with the physical and mechanical properties of the model materials applied in the experiments.
Peter Obermeier, Florian Duschl, and Michael C. Drews
Solid Earth, 16, 425–440, https://doi.org/10.5194/se-16-425-2025, https://doi.org/10.5194/se-16-425-2025, 2025
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We investigate geophysical properties and the distribution of vertical stress, which is defined by the weight of the rock column above a certain location in the subsurface, in the upper 5 km of the North Alpine Foreland Basin in Germany. Our results help us to understand the present-day geological configuration and to improve safety for subsurface use, such as deep geothermal energy production in the study area.
Gabriele Benedetti, Stefano Casiraghi, Daniela Bertacchi, and Andrea Bistacchi
Solid Earth, 16, 367–390, https://doi.org/10.5194/se-16-367-2025, https://doi.org/10.5194/se-16-367-2025, 2025
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At any scale, the limited size of a study area introduces a bias in the interpretation of linear features, defined as right-censoring bias. We show the effects of not considering such bias and apply survival analysis techniques to obtain unbiased estimates of multiple parametrical distributions in three censored length datasets. Finally, we propose a novel approach to select the most representative model from a sensible candidate pool using the probability integral transform technique.
Simone Masoch, Giorgio Pennacchioni, Michele Fondriest, Rodrigo Gomila, Piero Poli, José Cembrano, and Giulio Di Toro
Solid Earth, 16, 23–43, https://doi.org/10.5194/se-16-23-2025, https://doi.org/10.5194/se-16-23-2025, 2025
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We investigate an exhumed hydrothermal system in the Atacama Desert (Chile) to understand how earthquake swarms form. Wall rocks near fault veins experienced high-stress pulses, and fault veins underwent cyclic crack opening and shearing. These findings suggest ancient earthquake swarm activity, from dynamic crack propagation to repeated crack opening and shearing. This system represents a unique geological record of earthquake swarms, providing insights into their initiation and evolution.
Michał P. Michalak, Janusz Morawiec, and Peter Menzel
EGUsphere, https://doi.org/10.5194/egusphere-2024-3327, https://doi.org/10.5194/egusphere-2024-3327, 2025
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This study analyzes geological faults using triangular surface data to model displaced horizons, considering scenarios with and without elevation uncertainties. Formal proofs and computational experiments show that without elevation errors, identical dip directions occur. Even with uncertainties, the expected dip direction remains consistent. The findings offer insights for predicting fault geometry in data-sparse environments, improving fault modeling with imprecise elevation data.
Natalia Nevskaya, Alfons Berger, Holger Stünitz, Weijia Zhan, Markus Ohl, Oliver Plümper, and Marco Herwegh
EGUsphere, https://doi.org/10.5194/egusphere-2024-3968, https://doi.org/10.5194/egusphere-2024-3968, 2025
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Rheology of polymineralic rocks is crucial to unravel the strain and stress distribution in Earth’s middle crust with implications for e.g. seismicity or geothermal systems. Our experimental study of the viscous rheology of natural, fine-grained, granitoid rocks shows that dissolution-precipitation creep and pinning is active in extremely weak narrow zones. Due to the polymineralic character, strain localizes with and without a precursory fracture in zones weaker than monomineralic quartz.
Anthony Adwan, Bertrand Maillot, Pauline Souloumiac, Christophe Barnes, Christophe Nussbaum, Meinert Rahn, and Thomas Van Stiphout
Solid Earth, 15, 1445–1463, https://doi.org/10.5194/se-15-1445-2024, https://doi.org/10.5194/se-15-1445-2024, 2024
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We use computer simulations to study how stress is distributed in large-scale geological models, focusing on how fault lines behave under pressure. By running many 2D and 3D simulations with varying conditions, we discover patterns in how faults form and interact. Our findings reveal that even small changes in conditions can lead to different stress outcomes. This research helps us better understand earthquake mechanics and could improve predictions of fault behavior in real-world scenarios.
Pramit Chatterjee, Arnab Roy, and Nibir Mandal
Solid Earth, 15, 1281–1301, https://doi.org/10.5194/se-15-1281-2024, https://doi.org/10.5194/se-15-1281-2024, 2024
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Understanding strain accumulation processes in shear zones is essential for explaining failure mechanisms at great crustal depths. This study explores the rheological and kinematic factors determining the varying modes of shear accommodation in natural shear zones. Numerical simulations suggest that an interplay of parameters – initial viscosity, bulk shear rate, and internal cohesion – governs the dominance of one accommodation mechanism over another.
Jeffrey M. Rahl, Brendan Moehringer, Kenneth S. Befus, and John S. Singleton
Solid Earth, 15, 1233–1240, https://doi.org/10.5194/se-15-1233-2024, https://doi.org/10.5194/se-15-1233-2024, 2024
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At the high temperatures present in the deeper crust, minerals such as quartz can flow much like silly putty. The detailed mechanisms of how atoms are reorganized depends upon several factors, such as the temperature and the rate of which the mineral changes shape. We present observations from a naturally deformed rock showing that the amount of water present also influences the type of deformation in quartz, with implications for geological interpretations.
Malte Froemchen, Ken J. W. McCaffrey, Mark B. Allen, Jeroen van Hunen, Thomas B. Phillips, and Yueren Xu
Solid Earth, 15, 1203–1231, https://doi.org/10.5194/se-15-1203-2024, https://doi.org/10.5194/se-15-1203-2024, 2024
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The Shanxi Rift is a young, active rift in northern China that formed atop a Proterozoic orogen. The impact of these structures on active rift faults is poorly understood. Here, we quantify the landscape response to active faulting and compare it with published maps of inherited structures. We find that inherited structures played an important role in the segmentation of the Shanxi Rift and in the development of rift interaction zones, which are the most active regions in the Shanxi Rift.
Jinbao Su, Wenbin Zhu, and Guangwei Li
Solid Earth, 15, 1133–1141, https://doi.org/10.5194/se-15-1133-2024, https://doi.org/10.5194/se-15-1133-2024, 2024
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The late Mesozoic igneous rocks in the South China Block exhibit flare-ups and lulls, which form in compressional or extensional backgrounds. The ascending of magma forms a mush-like head and decreases crustal thickness. The presence of faults and pre-existing magmas will accelerate emplacement of underplating magma. The magmatism at different times may be formed under similar subduction conditions, and the boundary compression forces will delay magma ascent.
Peter Achtziger-Zupančič, Alberto Ceccato, Alba Simona Zappone, Giacomo Pozzi, Alexis Shakas, Florian Amann, Whitney Maria Behr, Daniel Escallon Botero, Domenico Giardini, Marian Hertrich, Mohammadreza Jalali, Xiaodong Ma, Men-Andrin Meier, Julian Osten, Stefan Wiemer, and Massimo Cocco
Solid Earth, 15, 1087–1112, https://doi.org/10.5194/se-15-1087-2024, https://doi.org/10.5194/se-15-1087-2024, 2024
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We detail the selection and characterization of a fault zone for earthquake experiments in the Fault Activation and Earthquake Ruptures (FEAR) project at the Bedretto Lab. FEAR, which studies earthquake processes, overcame data collection challenges near faults. The fault zone in Rotondo granite was selected based on geometry, monitorability, and hydro-mechanical properties. Remote sensing, borehole logging, and geological mapping were used to create a 3D model for precise monitoring.
Maxime Jamet, Gregory Ballas, Roger Soliva, Olivier Gerbeaud, Thierry Lefebvre, Christine Leredde, and Didier Loggia
Solid Earth, 15, 895–920, https://doi.org/10.5194/se-15-895-2024, https://doi.org/10.5194/se-15-895-2024, 2024
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This study characterizes the Tchirezrine II sandstone reservoir in northern Niger. Crucial for potential uranium in situ recovery (ISR), our multifaceted approach reveals (i) a network of homogeneously distributed orthogonal structures, (ii) the impact of clustered E–W fault structures on anisotropic fluid flow, and (iii) local changes in the matrix behaviour of the reservoir as a function of the density and nature of the deformation structure.
Matthew S. Hodge, Guri Venvik, Jochen Knies, Roelant van der Lelij, Jasmin Schönenberger, Øystein Nordgulen, Marco Brönner, Aziz Nasuti, and Giulio Viola
Solid Earth, 15, 589–615, https://doi.org/10.5194/se-15-589-2024, https://doi.org/10.5194/se-15-589-2024, 2024
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Smøla island, in the mid-Norwegian margin, has complex fracture and fault patterns resulting from tectonic activity. This study uses a multiple-method approach to unravel Smøla's tectonic history. We found five different phases of deformation related to various fracture geometries and minerals dating back hundreds of millions of years. 3D models of these features visualise these structures in space. This approach may help us to understand offshore oil and gas reservoirs hosted in the basement.
Karsten Reiter, Oliver Heidbach, and Moritz O. Ziegler
Solid Earth, 15, 305–327, https://doi.org/10.5194/se-15-305-2024, https://doi.org/10.5194/se-15-305-2024, 2024
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It is generally assumed that faults have an influence on the stress state of the Earth’s crust. It is questionable whether this influence is still present far away from a fault. Simple numerical models were used to investigate the extent of the influence of faults on the stress state. Several models with different fault representations were investigated. The stress fluctuations further away from the fault (> 1 km) are very small.
Yukinojo Koyama, Simon R. Wallis, and Takayoshi Nagaya
Solid Earth, 15, 143–166, https://doi.org/10.5194/se-15-143-2024, https://doi.org/10.5194/se-15-143-2024, 2024
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Stress along a subduction plate boundary is important for understanding subduction phenomena such as earthquakes. We estimated paleo-stress using quartz recrystallized grain size combined with deformation temperature and P–T paths of exhumed rocks. The obtained results show differential stresses of 30.8–82.7 MPa consistent over depths of 17–27 km in the paleo-subduction boundary. The obtained stress may represent the initial conditions under which slow earthquakes nucleated in the same domain.
Annelotte Weert, Kei Ogata, Francesco Vinci, Coen Leo, Giovanni Bertotti, Jerome Amory, and Stefano Tavani
Solid Earth, 15, 121–141, https://doi.org/10.5194/se-15-121-2024, https://doi.org/10.5194/se-15-121-2024, 2024
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On the road to a sustainable planet, geothermal energy is considered one of the main substitutes when it comes to heating. The geological history of an area can have a major influence on the application of these geothermal systems, as demonstrated in the West Netherlands Basin. Here, multiple episodes of rifting and subsequent basin inversion have controlled the distribution of the reservoir rocks, thus influencing the locations where geothermal energy can be exploited.
Pâmela C. Richetti, Frank Zwaan, Guido Schreurs, Renata S. Schmitt, and Timothy C. Schmid
Solid Earth, 14, 1245–1266, https://doi.org/10.5194/se-14-1245-2023, https://doi.org/10.5194/se-14-1245-2023, 2023
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The Araripe Basin in NE Brazil was originally formed during Cretaceous times, as South America and Africa broke up. The basin is an important analogue to offshore South Atlantic break-up basins; its sediments were uplifted and are now found at 1000 m height, allowing for studies thereof, but the cause of the uplift remains debated. Here we ran a series of tectonic laboratory experiments that show how a specific plate tectonic configuration can explain the evolution of the Araripe Basin.
Adam J. Cawood, Hannah Watkins, Clare E. Bond, Marian J. Warren, and Mark A. Cooper
Solid Earth, 14, 1005–1030, https://doi.org/10.5194/se-14-1005-2023, https://doi.org/10.5194/se-14-1005-2023, 2023
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Here we test conceptual models of fracture development by investigating fractures across multiple scales. We find that most fractures increase in abundance towards the fold hinge, and we interpret these as being fold related. Other fractures at the site show inconsistent orientations and are unrelated to fold formation. Our results show that predicting fracture patterns requires the consideration of multiple geologic variables.
Johanna Heeb, David Healy, Nicholas E. Timms, and Enrique Gomez-Rivas
Solid Earth, 14, 985–1003, https://doi.org/10.5194/se-14-985-2023, https://doi.org/10.5194/se-14-985-2023, 2023
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Hydration of rocks is a key process in the Earth’s crust and mantle that is accompanied by changes in physical traits and mechanical behaviour of rocks. This study assesses the influence of stress on hydration reaction kinetics and mechanics in experiments on anhydrite. We show that hydration occurs readily under stress and results in localized hydration along fractures and mechanic weakening. New gypsum growth is selective and depends on the stress field and host anhydrite crystal orientation.
Roy Helge Gabrielsen, Panagiotis Athanasios Giannenas, Dimitrios Sokoutis, Ernst Willingshofer, Muhammad Hassaan, and Jan Inge Faleide
Solid Earth, 14, 961–983, https://doi.org/10.5194/se-14-961-2023, https://doi.org/10.5194/se-14-961-2023, 2023
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The Barents Shear Margin defines the border between the relatively shallow Barents Sea that is situated on a continental plate and the deep ocean. This margin's evolution history was probably influenced by plate tectonic reorganizations. From scaled experiments, we deduced several types of structures (faults, folds, and sedimentary basins) that help us to improve the understanding of the history of the opening of the North Atlantic.
Leslie Logan, Ervin Veress, Joel B. H. Andersson, Olof Martinsson, and Tobias E. Bauer
Solid Earth, 14, 763–784, https://doi.org/10.5194/se-14-763-2023, https://doi.org/10.5194/se-14-763-2023, 2023
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The Pahtohavare Cu ± Au deposits in the Kiruna mining district have a dubious timing of formation and have not been contextualized within an up-to-date tectonic framework. Structural mapping was carried out to reveal that the deposits are hosted in brittle structures that cut a noncylindrical, SE-plunging anticline constrained to have formed during the late-Svecokarelian orogeny. These results show that Cu ± Au mineralization formed more than ca. 80 Myr after iron oxide–apatite mineralization.
Alexandra Tamas, Dan M. Tamas, Gabor Tari, Csaba Krezsek, Alexandru Lapadat, and Zsolt Schleder
Solid Earth, 14, 741–761, https://doi.org/10.5194/se-14-741-2023, https://doi.org/10.5194/se-14-741-2023, 2023
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Tectonic processes are complex and often difficult to understand due to the limitations of surface or subsurface data. One such process is inversion tectonics, which means that an area initially developed in an extension (such as the opening of an ocean) is reversed to compression (the process leading to mountain building). In this research, we use a laboratory method (analogue modelling), and with the help of a sandbox, we try to better understand structures (folds/faults) related to inversion.
Elizabeth Parker Wilson, Pablo Granado, Pablo Santolaria, Oriol Ferrer, and Josep Anton Muñoz
Solid Earth, 14, 709–739, https://doi.org/10.5194/se-14-709-2023, https://doi.org/10.5194/se-14-709-2023, 2023
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This work focuses on the control of accommodation zones on extensional and subsequent inversion in salt-detached domains using sandbox analogue models. During extension, the transfer zone acts as a pathway for the movement of salt, changing the expected geometries. When inverted, the salt layer and syn-inversion sedimentation control the deformation style in the salt-detached cover system. Three natural cases are compared to the model results and show similar inversion geometries.
Oriol Ferrer, Eloi Carola, and Ken McClay
Solid Earth, 14, 571–589, https://doi.org/10.5194/se-14-571-2023, https://doi.org/10.5194/se-14-571-2023, 2023
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Using an experimental approach based on scaled sandbox models, this work aims to understand how salt above different rotational fault blocks influences the cover geometry and evolution, first during extension and then during inversion. The results show that inherited salt structures constrain contractional deformation. We show for the first time how welds and fault welds are reopened during contractional deformation, having direct implications for the subsurface exploration of natural resources.
Chiara Montemagni, Stefano Zanchetta, Martina Rocca, Igor M. Villa, Corrado Morelli, Volkmar Mair, and Andrea Zanchi
Solid Earth, 14, 551–570, https://doi.org/10.5194/se-14-551-2023, https://doi.org/10.5194/se-14-551-2023, 2023
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The Vinschgau Shear Zone (VSZ) is one of the largest and most significant shear zones developed within the Late Cretaceous thrust stack in the Austroalpine domain of the eastern Alps. 40Ar / 39Ar geochronology constrains the activity of the VSZ between 97 and 80 Ma. The decreasing vorticity towards the core of the shear zone, coupled with the younging of mylonites, points to a shear thinning behavior. The deepest units of the Eo-Alpine orogenic wedge were exhumed along the VSZ.
Jordi Miró, Oriol Ferrer, Josep Anton Muñoz, and Gianreto Manastchal
Solid Earth, 14, 425–445, https://doi.org/10.5194/se-14-425-2023, https://doi.org/10.5194/se-14-425-2023, 2023
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Using the Asturian–Basque–Cantabrian system and analogue (sandbox) models, this work focuses on the linkage between basement-controlled and salt-decoupled domains and how deformation is accommodated between the two during extension and subsequent inversion. Analogue models show significant structural variability in the transitional domain, with oblique structures that can be strongly modified by syn-contractional sedimentation. Experimental results are consistent with the case study.
Junichi Fukuda, Takamoto Okudaira, and Yukiko Ohtomo
Solid Earth, 14, 409–424, https://doi.org/10.5194/se-14-409-2023, https://doi.org/10.5194/se-14-409-2023, 2023
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We measured water distributions in deformed quartz by infrared spectroscopy mapping and used the results to discuss changes in water distribution resulting from textural development. Because of the grain size reduction process (dynamic recrystallization), water contents decrease from 40–1750 wt ppm in host grains of ~2 mm to 100–510 wt ppm in recrystallized regions composed of fine grains of ~10 µm. Our results indicate that water is released and homogenized by dynamic recrystallization.
Bastien Walter, Yves Géraud, Alexiane Favier, Nadjib Chibati, and Marc Diraison
EGUsphere, https://doi.org/10.5194/egusphere-2023-397, https://doi.org/10.5194/egusphere-2023-397, 2023
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Lake Abhe in southwestern Djibouti is known for its exposures of massive hydrothermal chimneys and hot springs on the lake’s eastern shore. This study highlights the control of the main structural faults of the area on the development of these hydrothermal features. This work contributes to better understand hydrothermal fluid pathways in this area and may help further exploration for the geothermal development of this remarkable site.
Michael Rudolf, Matthias Rosenau, and Onno Oncken
Solid Earth, 14, 311–331, https://doi.org/10.5194/se-14-311-2023, https://doi.org/10.5194/se-14-311-2023, 2023
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Analogue models of tectonic processes rely on the reproduction of their geometry, kinematics and dynamics. An important property is fault behaviour, which is linked to the frictional characteristics of the fault gouge. This is represented by granular materials, such as quartz sand. In our study we investigate the time-dependent frictional properties of various analogue materials and highlight their impact on the suitability of these materials for analogue models focusing on fault reactivation.
Jessica Barabasch, Joyce Schmatz, Jop Klaver, Alexander Schwedt, and Janos L. Urai
Solid Earth, 14, 271–291, https://doi.org/10.5194/se-14-271-2023, https://doi.org/10.5194/se-14-271-2023, 2023
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We analysed Zechstein salt with microscopes and observed specific microstructures that indicate much faster deformation in rock salt with fine halite grains when compared to salt with larger grains. This is important because people build large cavities in the subsurface salt for energy storage or want to deposit radioactive waste inside it. When engineers and scientists use grain-size data and equations that include this mechanism, it will help to make better predictions in geological models.
Nicolás Molnar and Susanne Buiter
Solid Earth, 14, 213–235, https://doi.org/10.5194/se-14-213-2023, https://doi.org/10.5194/se-14-213-2023, 2023
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Progression of orogenic wedges over pre-existing extensional structures is common in nature, but deciphering the spatio-temporal evolution of deformation from the geological record remains challenging. Our laboratory experiments provide insights on how horizontal stresses are transferred across a heterogeneous crust, constrain which pre-shortening conditions can either favour or hinder the reactivatation of extensional structures, and explain what implications they have on critical taper theory.
Tania Habel, Martine Simoes, Robin Lacassin, Daniel Carrizo, and German Aguilar
Solid Earth, 14, 17–42, https://doi.org/10.5194/se-14-17-2023, https://doi.org/10.5194/se-14-17-2023, 2023
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The Central Andes are one of the most emblematic reliefs on Earth, but their western flank remains understudied. Here we explore two rare key sites in the hostile conditions of the Atacama desert to build cross-sections, quantify crustal shortening, and discuss the timing of this deformation at ∼20–22°S. We propose that the structures of the Western Andes accommodated significant crustal shortening here, but only during the earliest stages of mountain building.
Naïm Célini, Frédéric Mouthereau, Abdeltif Lahfid, Claude Gout, and Jean-Paul Callot
Solid Earth, 14, 1–16, https://doi.org/10.5194/se-14-1-2023, https://doi.org/10.5194/se-14-1-2023, 2023
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We investigate the peak temperature of sedimentary rocks of the SW Alps (France), using Raman spectroscopy on carbonaceous material. This method provides an estimate of the peak temperature achieved by organic-rich rocks. To determine the timing and the tectonic context of the origin of these temperatures we use 1D thermal modelling. We find that the high temperatures up to 300 °C were achieved during precollisional extensional events, not during tectonic burial in the Western Alps.
Luke N. J. Wedmore, Tess Turner, Juliet Biggs, Jack N. Williams, Henry M. Sichingabula, Christine Kabumbu, and Kawawa Banda
Solid Earth, 13, 1731–1753, https://doi.org/10.5194/se-13-1731-2022, https://doi.org/10.5194/se-13-1731-2022, 2022
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Mapping and compiling the attributes of faults capable of hosting earthquakes are important for the next generation of seismic hazard assessment. We document 18 active faults in the Luangwa Rift, Zambia, in an active fault database. These faults are between 9 and 207 km long offset Quaternary sediments, have scarps up to ~30 m high, and are capable of hosting earthquakes from Mw 5.8 to 8.1. We associate the Molaza Fault with surface ruptures from two unattributed M 6+ 20th century earthquakes.
Michał P. Michalak, Lesław Teper, Florian Wellmann, Jerzy Żaba, Krzysztof Gaidzik, Marcin Kostur, Yuriy P. Maystrenko, and Paulina Leonowicz
Solid Earth, 13, 1697–1720, https://doi.org/10.5194/se-13-1697-2022, https://doi.org/10.5194/se-13-1697-2022, 2022
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When characterizing geological/geophysical surfaces, various geometric attributes are calculated, such as dip angle (1D) or dip direction (2D). However, the boundaries between specific values may be subjective and without optimization significance, resulting from using default color palletes. This study proposes minimizing cosine distance among within-cluster observations to detect 3D anomalies. Our results suggest that the method holds promise for identification of megacylinders or megacones.
Erik M. Young, Christie D. Rowe, and James D. Kirkpatrick
Solid Earth, 13, 1607–1629, https://doi.org/10.5194/se-13-1607-2022, https://doi.org/10.5194/se-13-1607-2022, 2022
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Studying how earthquakes spread deep within the faults they originate from is crucial to improving our understanding of the earthquake process. We mapped preserved ancient earthquake surfaces that are now exposed in South Africa and studied their relationship with the shape and type of rocks surrounding them. We determined that these surfaces are not random and are instead associated with specific kinds of rocks and that their shape is linked to the evolution of the faults in which they occur.
Sivaji Lahiri, Kitty L. Milliken, Peter Vrolijk, Guillaume Desbois, and Janos L. Urai
Solid Earth, 13, 1513–1539, https://doi.org/10.5194/se-13-1513-2022, https://doi.org/10.5194/se-13-1513-2022, 2022
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Understanding the mechanism of mechanical compaction is important. Previous studies on mechanical compaction were mostly done by performing experiments. Studies on natural rocks are rare due to compositional heterogeneity of the sedimentary succession with depth. Due to remarkable similarity in composition and grain size, the Sumatra subduction complex provides a unique opportunity to study the micromechanism of mechanical compaction on natural samples.
Dongwon Lee, Nikolaos Karadimitriou, Matthias Ruf, and Holger Steeb
Solid Earth, 13, 1475–1494, https://doi.org/10.5194/se-13-1475-2022, https://doi.org/10.5194/se-13-1475-2022, 2022
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This research article focuses on filtering and segmentation methods employed in high-resolution µXRCT studies for crystalline rocks, bearing fractures, or fracture networks, of very small aperture. Specifically, we focus on the identification of artificially induced (via quenching) fractures in Carrara marble samples. Results from the same dataset from all five different methods adopted were produced and compared with each other in terms of their output quality and time efficiency.
Alberto Ceccato, Giulia Tartaglia, Marco Antonellini, and Giulio Viola
Solid Earth, 13, 1431–1453, https://doi.org/10.5194/se-13-1431-2022, https://doi.org/10.5194/se-13-1431-2022, 2022
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The Earth's surface is commonly characterized by the occurrence of fractures, which can be mapped, and their can be geometry quantified on digital representations of the surface at different scales of observation. Here we present a series of analytical and statistical tools, which can aid the quantification of fracture spatial distribution at different scales. In doing so, we can improve our understanding of how fracture geometry and geology affect fluid flow within the fractured Earth crust.
Giulio Viola, Giovanni Musumeci, Francesco Mazzarini, Lorenzo Tavazzani, Manuel Curzi, Espen Torgersen, Roelant van der Lelij, and Luca Aldega
Solid Earth, 13, 1327–1351, https://doi.org/10.5194/se-13-1327-2022, https://doi.org/10.5194/se-13-1327-2022, 2022
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A structural-geochronological approach helps to unravel the Zuccale Fault's architecture. By mapping its internal structure and dating some of its fault rocks, we constrained a deformation history lasting 20 Myr starting at ca. 22 Ma. Such long activity is recorded by now tightly juxtaposed brittle structural facies, i.e. different types of fault rocks. Our results also have implications on the regional evolution of the northern Apennines, of which the Zuccale Fault is an important structure.
Wan-Lin Hu
Solid Earth, 13, 1281–1290, https://doi.org/10.5194/se-13-1281-2022, https://doi.org/10.5194/se-13-1281-2022, 2022
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Having a seismic image is generally expected to enable us to better determine fault geometry and thus estimate geological slip rates accurately. However, the process of interpreting seismic images may introduce unintended uncertainties, which have not yet been widely discussed. Here, a case of a shear fault-bend fold in the frontal Himalaya is used to demonstrate how differences in interpretations can affect the following estimates of slip rates and dependent conclusions.
Manuel D. Menzel, Janos L. Urai, Estibalitz Ukar, Thierry Decrausaz, and Marguerite Godard
Solid Earth, 13, 1191–1218, https://doi.org/10.5194/se-13-1191-2022, https://doi.org/10.5194/se-13-1191-2022, 2022
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Mantle rocks can bind large quantities of carbon by reaction with CO2, but this capacity requires fluid pathways not to be clogged by carbonate. We studied mantle rocks from Oman to understand the mechanisms allowing their transformation into carbonate and quartz. Using advanced imaging techniques, we show that abundant veins were essential fluid pathways driving the reaction. Our results show that tectonic stress was important for fracture opening and a key ingredient for carbon fixation.
Jean-Baptiste P. Koehl, Steffen G. Bergh, and Arthur G. Sylvester
Solid Earth, 13, 1169–1190, https://doi.org/10.5194/se-13-1169-2022, https://doi.org/10.5194/se-13-1169-2022, 2022
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The San Andreas fault is a major active fault associated with ongoing earthquake sequences in southern California. The present study investigates the development of the Indio Hills area in the Coachella Valley along the main San Andreas fault and the Indio Hills fault. The Indio Hills area is located near an area with high ongoing earthquake activity (Brawley seismic zone), and, therefore, its recent tectonic evolution has implications for earthquake prediction.
Jin Lai, Dong Li, Yong Ai, Hongkun Liu, Deyang Cai, Kangjun Chen, Yuqiang Xie, and Guiwen Wang
Solid Earth, 13, 975–1002, https://doi.org/10.5194/se-13-975-2022, https://doi.org/10.5194/se-13-975-2022, 2022
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(1) Structural diagenesis analysis is performed on the ultra-deep tight sandstone. (2) Fracture and intergranular pores are related to the low in situ stress magnitudes. (3) Dissolution is associated with the presence of fracture.
Hamed Fazlikhani, Wolfgang Bauer, and Harald Stollhofen
Solid Earth, 13, 393–416, https://doi.org/10.5194/se-13-393-2022, https://doi.org/10.5194/se-13-393-2022, 2022
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Interpretation of newly acquired FRANKEN 2D seismic survey data in southeeastern Germany shows that upper Paleozoic low-grade metasedimentary rocks and possible nappe units are transported by Variscan shear zones to ca. 65 km west of the Franconian Fault System (FFS). We show that the locations of post-Variscan upper Carboniferous–Permian normal faults and associated graben and half-graben basins are controlled by the geometry of underlying Variscan shear zones.
Xiaodong Ma, Marian Hertrich, Florian Amann, Kai Bröker, Nima Gholizadeh Doonechaly, Valentin Gischig, Rebecca Hochreutener, Philipp Kästli, Hannes Krietsch, Michèle Marti, Barbara Nägeli, Morteza Nejati, Anne Obermann, Katrin Plenkers, Antonio P. Rinaldi, Alexis Shakas, Linus Villiger, Quinn Wenning, Alba Zappone, Falko Bethmann, Raymi Castilla, Francisco Seberto, Peter Meier, Thomas Driesner, Simon Loew, Hansruedi Maurer, Martin O. Saar, Stefan Wiemer, and Domenico Giardini
Solid Earth, 13, 301–322, https://doi.org/10.5194/se-13-301-2022, https://doi.org/10.5194/se-13-301-2022, 2022
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Questions on issues such as anthropogenic earthquakes and deep geothermal energy developments require a better understanding of the fractured rock. Experiments conducted at reduced scales but with higher-resolution observations can shed some light. To this end, the BedrettoLab was recently established in an existing tunnel in Ticino, Switzerland, with preliminary efforts to characterize realistic rock mass behavior at the hectometer scale.
Berit Schwichtenberg, Florian Fusseis, Ian B. Butler, and Edward Andò
Solid Earth, 13, 41–64, https://doi.org/10.5194/se-13-41-2022, https://doi.org/10.5194/se-13-41-2022, 2022
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Hydraulic rock properties such as porosity and permeability are relevant factors that have an impact on groundwater resources, geological repositories and fossil fuel reservoirs. We investigate the influence of chemical compaction upon the porosity evolution in salt–biotite mixtures and related transport length scales by conducting laboratory experiments in combination with 4-D analysis. Our observations invite a renewed discussion of the effect of sheet silicates on chemical compaction.
Cited articles
Accordi, G.: Il reticolo dei Monti Martani, B. Soc. Geol. Ital., 95, 3–26, 1966.
Alfonsini, L.: Wrench tectonic in Central Italy, a segment of the Sabina Fauls, B. Soc. Geol. Ital., 114, 414–421, 1995.
Alfonsini, L., Funiciello, R., Mattei, M., Girotti, O., Maiorani, A., Preite Martinez, M., Trudu, C., and Turi, B.: Structural and geochemical features of the Sabina strike-slip fault (Central Apennines), B. Soc. Geol. Ital., 110, 207–230, 1991.
Ambrosetti, P., Carboni, M. G., Conti, M. A., Costantini, A., Esu, D., Gandin, A., Girotti, O., Lazzarotto, A., Mazzanti, R., Nicosia, U., Parisi, G., and Sandrelli, F.: Evoluzione paleogeografica e tettonica dei bacini tosco-umbro-laziali nel Pliocene e nel Pleistocene inferiore, Memorie della Società Geologica Italiana, 19, 573–580, 1978.
Ambrosetti, P., Carboni, M. G., Conti, M. A., Esu, D., Girotti, O., La Monica, G. B., Landini, B., and Parisi, G.: Il Pliocene ed il Pleistocene inferiore del bacino del Fiume Tevere nell'Umbria meridionale: The Pliocene and the Lower Pleistocene of the Tevere Basin in Southern Umbria, Geogr. Fis. Din. Quat., 10, 10–33, 1987a.
Ambrosetti, P., Bosi, C., Carraro, F., Ciaranfi, N., Panizza, M., Papani, G., Vezzani, L., and Zanferrari, A.: Neotectonic Map of Italy: Scale 1:500000, Consiglio Nazionale delle Ricerche, Progetto Finalizzato Geodinamica, Sottoprogetto Neotettonica. Litografia Artistica Cartografica, Florence (Italy), 1987b.
Angelier, J. and Mechler, P.: Sur une méthode graphique de recherche des contraintes principales également utilisable en tectonique et en seismologie: la méthode des dièdres droits, B. Soc. Geol. Fr., 7-XIX, 1309–1318, 1977.
Aringoli, D., Farabollini, P., Gentili, B., Materazzi, M., and Pambianchi G.: Geomorphological evidences of natural disasters in the roman archaeological site of Carsulae (Tiber basin, Central Italy), in: Ol' man river: Geo-Archaelogical Aspects of Rivers and River plains, Ghent, edited by: de Dapper, M., Vermeulen, F., Deprez, S., and Taelman, D., Academia Press, 5–20, ISBN 9789038214047, 2009.
Autin, J., Bellahsen, N., Leroy, S., Husson, L., Beslier, M. O., and d'Acremont, E.: The role of structural inheritance in oblique rifting: Insights from analogue models and application to the Gulf of Aden, Tectonophysics, 607, 51–64, https://doi.org/10.1016/j.tecto.2013.05.041, 2013.
Barchi, M.: Una sezione geologica bilanciata attraverso il settore meridionale dell'Appennino umbro-marchigiano: l'Acquasparta-Spoleto-Accumuli, Studi Geologici Camerti, Vol. Spec. 1991/1, CROP 03, 347–362, 1991.
Barchi, M.: The Neogene–Quaternary evolution of the Northern Apennines: Crustal structure, style of deformation and seismicity, J. Virtual Explor, 36, 1–24, 2010.
Barchi, M., Brozzetti, F., and Lavecchia, G.: Analisi strutturale e geometria dei bacini della media valle del Tevere e della Valle Umbra, B. Soc. Geol. Ital., 110, 65–76, 1991.
Barchi, M., Carboni, F., Michele, M., Ercoli, M., Giorgetti, C., Porreca, M., Azzaro, S., and Chiaraluce, L.: The influence of subsurface geology on the distribution of earthquakes during the 2016–2017 Central Italy seismic sequence, Tectonophysics, 807, 228797, https://doi.org/10.1016/j.tecto.2021.228797, 2021.
Basilici, G.: II Bacino continentale Tiberino (Plio–Pleistocene, Umbria): analisi sedimentologica e stratigralica, PhD thesis, University of Bologna, 323 pp., 1992.
Basilici, G.: Evoluzione deposizionale del ramo sud-occidentale del Bacino Tiberino (Plio–Pleistocene, Umbria): da un sistema lacustre profondo as una piana alluvionale, Abstract for the conference: Le Conche Intermontane, 13–15 September 1993, Rome, 11–13, https://amq.aiqua.it/index.php/amq/article/view/1307 (last access: 20 December 2024), 1993.
Basilici, G.: Sedimentary facies in an extensional and deep-lacustrine depositional system: the Pliocene Tiberino Basin, Central Italy, Sediment. Geol., 109, 73–94, 1997.
Bernoulli, D., Kälin, O., and Patacca, E.: A sunken continental margin of the Mesozoic Tethys: The northern and central Apennines, in: Symposium: “Sédimentation Jurassique W européen”, 1977, Paris, Vol. 1, edited by: Beaudoin, B. and Purser, B. H., Publication Spécial Association Sédimentologique Française, 197–210, https://www.sedimentologie.fr/edition/la-sedimentation-du-jurassique-w-europeen/ (last access: 19 December 2024), 1979.
Berthé, D., Choukroune, P., and Jegouzo, P.: Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear Zone, J. Struct. Geol., 1, 31–42, 1979.
Boccaletti, M. and Guazzone, G.: Remnant arcs and marginal basins in the Cainozoic development of the Mediterranean, Nature, 252, 18–21, 1974.
Boccaletti, M., Elter, P., and Guazzone, G.: Plate tectonic models for the development of the Western Alps and Northern Apennines, Nature, 234, 108–111, 1971.
Boccaletti, M., Coli, M., Eva, C., Ferrari, G., Giglia, G., Lazzarotto, A., Merlanti, F., Nicolich, R., Papani, G., and Postpischl, D.: Considerations on the seismotectonics of the Northern Apennines, Tectonophysics, 117, 7–38, 1985.
Boncio, P., Brozzetti, F., and Lavecchia, G.: Architecture and seismotectonics of a regional low-angle normal fault zone in Central Italy, Tectonics, 19, 1038–1055, 2000.
Bonini, M.: Chronology of deformation and analogue modelling of the Plio–Pleistocene `Tiber Basin': implications for the evolution of the Northern Apennines (Italy), Tectonophysics, 285, 147–165, 1998.
Bonini, M., Tanini, C., Moratti, G., Piccardi, L., and Sani, F.: Geological and archaeological evidence of active faulting on the Martana Fault (Umbria–Marche Apennines, Italy) and its geodynamic implications, J. Quaternary Sci., 18, 695–708, 2003.
Bottari, C. and Sepe, V.: The role of earthquakes, landslides and climate changes in the abandonment of the Roman Carsulae site (Tevere basin e Central Italy), Quatern. Int., 308–309, 105–111, 2013.
Bottari, C., Aringoli, D., Carluccio, R., Castellano, C., Caracciolo, F. A., Gasperini, M., Materazzi, M., Nicolosi, I., Pambianchi, G., Pieruccini, P., and Sepe, V.: Geomorphological and geophysical investigations for the characterization of the Roman Carsulae site (Tiber basin, Central Italy), J. Appl. Geophys., 143, 74–85, https://doi.org/10.1016/j.jappgeo.2017.03.021, 2017.
Brozzetti, F. and Lavecchia, G.: Evoluzione del campo degli sforzi e storia deformativa nell'area dei Monti Martani (Umbria), B. Soc. Geol. Ital., 114, 155–176, 1995.
Brozzetti, F. and Stoppa, F.: Le piroclastiti medio-pleistoceniche di Massa Martana-Acquasparta (Umbria): caratteri strutturali e vulcanologici, Il Quaternario, 8, 95–110, 1995.
Brune, S.: Evolution of stress and fault patterns in oblique rift systems: 3-D numerical lithospheric-scale experiments from rift to breakup, Geochem. Geophy. Geosy., 15, 3392–3415, https://doi.org/10.1002/2014GC005446, 2014.
Brune, S.: Rifts and rifted margins: a review of geodynamic processes and natural hazards, in: Plate Boundaries and Natural Hazards, vol. 219, edited by: Duarte, J. C. and Schellart, W. P., Geophysical Monograph Series, Am. Geophys. Un., https://doi.org/10.1002/9781119054146.ch2, 2016.
Bruni, F., Calamita, F., Maranci, M., and Pierantoni, P. P.: Il controllo della tettonica giurassica sulla strutturazione neogenica dei Monti Martani meridionali (Preappennino umbro), Studi Geologici Camerti, Vol. Spec. 1995/1, 121–135, 1995.
Butler, H. R. W., Mazzoli, S., Corrado, S., Donatis, M. D., Bucci, D. D., Gambini, R., Naso, G., Nicolai, C., Scrocca, D., Shiner, P., and Zucconi, V.: Applying thick-skinned tectonic models to the Apennine thrust belt of Italy—Limitations and implications, in: Thrust tectonics and hydrocarbon systems, edited by: McClay, M. C. R., AAPG, https://doi.org/10.1306/m82813c34, 2004.
Butler, R. W. H., Tavarnelli, E., and Grasso, M.: Structural inheritance in mountain belts: an Alpine–Apennine perspective, J. Struct. Geol., 28, 1893–908, 2006.
Buttinelli, M., Pezzo, G., Valoroso, L., De Gori, P., and Chiarabba, C.: Tectonics inversions, fault segmentation, and triggering mechanisms in the central Apennines normal fault system: Insights from high-resolution velocity models, Tectonics, 37, 4135–4149, https://doi.org/10.1029/2018TC005053, 2018.
Calamita, F. and Pierantoni, P. P.: Structural setting of the Southern Martani Mountains (Umbria Apennines: Central Italy), Memorie della Società Geologica Italiana, 48, 549–557, 1994.
Calamita, F. and Pierantoni, P. P.: Modalità della strutturazione neogenica nell'Appennino Umbro-Sabino (Italia Centrale), Studi Geologici Camerti, Vol. Spec. 1995/1, 153–169, 1995.
Calamita, F., Cello, G., Centamore, E., Deiana, G., Micarelli, A., Paltrinieri, W., and Ridolfi, M.: Stile deformativo e cronologia della deformazione lungo tre sezioni bilanciate dall'Appennino umbro-marchigiano alla costa adriatica, Studi Geologici Camerti, Vol. Spec. 1991/1, 295–314, 1991.
Calamita, F., Satolli, S., Scisciani, V., Esestime, P., and Pace, P.: Contrasting styles of fault reactivation in curved orogenic belts: Examples from the central Apennines (Italy), Geol. Soc. Am. Bull., 123, 1097–1111, 2011.
Capotorti, F. and Muraro, C.: Post-rift extensional tectonics at the edge of a carbonate platform: insights from the Middle Jurassic–Early Cretaceous Monte Giano stratigraphic record (central Apennines, Italy), Geol. Acta, 19, 0012, 2021.
Capotorti, F. and Muraro, C.: Jurassic to Quaternary reactivation of inherited structures in the central Apennines, Ital. J. Geosci., 143, 37–59, 2024.
Cardello, G. L. and Doglioni, C.: From Mesozoic rifting to Apennine orogeny: The Gran Sasso range (Italy), Gondwana Res., 27, 1307–1334, https://doi.org/10.1016/j.gr.2014.09.009, 2015.
Caricchi, C., Cifelli, F., Sagnotti, L., Sani, F., Speranza, F., and Mattei M.: Paleomagnetic evidence for a post-Eocene 90° CCW rotation of internal Apennine units: A linkage with Corsica-Sardinia rotation?, Tectonics, 33, 374–392, https://doi.org/10.1002/2013TC003364, 2014.
Carminati, E., Lustrino, M., and Doglioni, C.: Geodynamic evolution of the central and western Mediterranean: Tectonics vs. igneous petrology constraints, Tectonophysics, 579, 173–192, 2012.
Castellarin, A., Colacicchi, R., and Praturlon, A.: Fasi distensive, trascorrenze e sovrascorrimenti lungo la 'linea Ancona-Anzio', dal Lias medio al Pliocene, Geologica Romana, 17, 161–189, 1978.
Cattuto, C., Gregori, L., Melelli, L., Taramelli, A., and Troiani, C.: Paleogeographic evolution of the Terni basin (Umbria, Italy), Proceedings of the Scientific Meeting `Geological and geodynamic evolution of the Apennines' in memory of Giampaolo Pialli, Foligno (PG), 16–17 February 2000, B. Soc. Geol. Ital., Special Volume 1, 865–872, 2002.
Cavinato, G. P. and De Celles, P. G.: Extensional basins in the tectonically bimodal central Apennines fold-thrust belt, Italy: response to corner flow above a subducting slab in retrograde motion, Geology, 27, 955–958, 1999.
Cello, G., Mazzoli, S., Tondi, E., and Turco, E.: Active tectonics in the Central Apennines and possible implications for seismic hazard analysis in peninsular Italy, Tectonophysics, 272, 43–68, 1997.
Centamore, E., Deiana, G., Micarelli, A., and Potetti, M.: Il Trias-Paleogene delle Marche, Studi Geologici Camerti, Volume speciale “La Geologia delle Marche”, 9–27, 1986.
Centamore, E., Di Manna, P., and Rossi, D.: Kinematic evolution of the Volsci Range: a new overview, B. Soc. Geol. Ital., 126, 159, 2007.
Chiarabba, C. and Amato, A.: Vp and Vp/Vs images in the Mw 6.0 Colfiorito fault region (central Italy): A contribution to the understanding of seismotectonic and seismogenic processes, J. Geophys. Res., 108, 2248, https://doi.org/10.1029/2001JB001665, 2003.
Cipriani, A. and Bottini, C.: Early Cretaceous tectonic rejuvenation of an Early Jurassic margin in the Central Apennines: The “Mt. Cosce Breccia”, Sediment. Geol., 387, 57–74, 2019a.
Cipriani, A. and Bottini, C.: Unconformities, neptunian dykes and mass-transport deposits as an evidence for Early Cretaceous syn-sedimentary tectonics: New insights from the Central Apennines, Ital. J. Geosci., 138, 333–354, 2019b.
Cipriani, A., Fabbi, S., Lathuilière, B., and Santantonio, M.: A reef coral in the condensed Maiolica facies on the Mt Nerone pelagic carbonate platform (Marche Apennines): The enigma of ancient pelagic deposits, Sediment. Geol., 385, 45–60, 2019.
Cipriani, A., Caratelli, M., and Santantonio, M.: Geological mapping reveals the role of Early Jurassic rift architecture in the dispersal of calciturbidites: New insights from the Central and Northern Apennines, Basin Res., 32, 1485–1509, https://doi.org/10.1111/bre.12438, 2020.
Coltorti, M. and Bosellini, A.: Sedimentazione e tettonica nel Giurassico della dorsale marchigiana, Studi Geologici Camerti, 6, 13–21, 1980.
Coltorti, M., Pierantoni, P. P., and Pieruccini, P.: I depositi fluvio-lacustri di Montebibico (Monti Martani meridionali) ed il loro significato nell'evoluzione tettonico-sedimentaria del Bacino Tiberino, Studi Geologici Camerti, Vol. Spec. 1995/1, 305–314, 1995.
Conti, M. A. and Girotti, O.: Il Villafranchiano del ”lago Tiberino”, ramo Sud occidentale. Schema stratigrafico e tettonico, Geologica Romana, 16, 67–80, 1977.
Conti, P., Cornamusini, G., Carmignani, L., Motti, A., Natali, N., Bettucci, C., Lavorini, G., Pirro, A., Pizziolo, M., and Daniele, G.: An outline of the geology of the Northern Apennines (Italy), with geological map at
Cosentino, D., Cipollari, P., Marsili, P., and Scrocca, D.: Geology of the Central Apennines: A regional review, in: The Geology of Italy, edited by: Beltrando, M., Peccerillo, A., Mattei, M., Conticelli, S., and Doglioni, C., Journal of the Virtual Explorer (Electronic Edition), 36, paper 11, 2010.
Cowie, P. A., Roberts, G. P., Bull, J. M., and Visini, F.: Relationships between fault geometry, slip rate variability and earthquake recurrence in extensional settings, Geophys. J. Int., 189, 143–160, https://doi.org/10.1111/j.1365-246X.2012.05378.x, 2012.
Curzi, M., Aldega, L., Bernasconi, S. M., Berra, F., Billi, A., Boschi, C., Franchini, S., van der Lelij, R., Viola, G., and Carminati, E.: Architecture and evolution of an extensionally-inverted thrust (Mt. Tancia Thrust, Central Apennines): Geological, structural, geochemical, and K–Ar geochronological constraints, J. Struct. Geol., 136, 104059, https://doi.org/10.1016/j.jsg.2020.104059, 2020.
Curzi, M., Cipriani, A., Aldega, L., Billi, A., Carminati, E., van der Lelij, R., Vignaroli, G., and Viola, G.: Architecture and permeability structure of the Sibillini Mts. Thrust and influence upon recent, extension-related seismicity in the central Apennines (Italy) through fault-valve behavior, Geol. Soc. Am. Bull., 136, 3–26, 2024.
Decandia, F. A. and Tavarnelli, E.: Cronologia delle deformazioni nell'area di Spoleto (Umbria sud-orientale), Studi Geologici Camerti, Vol. Spec. 1991/1, 329–331, 1991.
Delvaux, D.: The TENSOR program for paleostress reconstruction: exemples from the east African and the Baikal rift zones, EUG VII Strasbourg, France, 4–8 April 1993, Abstract supplement N.1 to Terra Nova, 5, 216, 1993.
Delvaux, D. and Sperner, B.: Stress tensor inversion from fault kinematic indicators and focal mechanism data: the TENSOR program, in: New Insights into Structural Interpretation and Modelling, edited by: Nieuwland, D., Geological Society of London Special Publication, 212, 75–100, 2003.
Del Ventisette, C., Bonini, M., Maestrelli, D., Sani, F., Iavarone, E., and Montanari, D.: 3D-thrust fault pattern control on negative inversion: An analogue modelling perspective on central Italy, J. Struct. Geol., 143, 104254, https://doi.org/10.1016/j.jsg.2020.104254, 2021.
Destro, N.: Release fault: a variety of cross fault in linked extensional fault systems in the Sergipe-Alagoas basin, northeast Brazil, J. Struct. Geol., 17, 615–629, 1995.
Destro, N., Szatmari, P., Alkmim, F. F., Magnavita, L. P.: Release faults, associated structures, and their control on petroleum trends in the Recôncavo rift, northeast Brazil, AAPG Bull., 87,1123–1144. https://doi.org/10.1306/02200300156, 2003.
Di Domenica, A., Turtù, A., Satolli, S., and Calamita, F.: Relationships between thrusts and normal faults in curved belts: New insight in the inversion tectonics of the central-northern Apennines (Italy), J. Struct. Geol., 42, 104–117, https://doi.org/10.1016/j.jsg.2012.06.008, 2012.
Doglioni, C., Gueguen, E., Harabaglia, P., and Mongelli, F.: On the origin of west-directed subduction zones and applications to the western Mediterranean, in: The Mediterranean basins: Tertiary ex-tension within the Alpine orogen, edited by: Durand, B., Jolivet, L., Horvath, F., and Seranne, M., Geological Society of London Special Publication, 156, 541–561, 1999.
Dramis, F.: Il ruolo dei sollevementi tettonici a largo raggio nella genesi del rilievo appenninico, Studi Geologici Camerti, 1992/1, 9–15, 1992.
Elter, P.: L'ensemble ligure, B. Soc. Geol. Fr., 17, 984—997, 1975.
Faccenna, C., Mattei, M., Funiciello, D., and Jolivet, L.: Styles of back-arc extension in the Central Mediterranean, Terra Nova, 9, 126–130, https://doi.org/10.1046/j.1365-3121.1997.d01-12.x, 1997.
Faccenna, C., Becker, T. W., Lucente, F. P., Jolivet, L., and Rossetti, F.: History of subduction and back arc extension in the Central Mediterranean, Geophys. J. Int., 145(3), 809–820, https://doi.org/10.1046/j.0956-540x.2001.01435.x, 2001.
Farinacci, A., Malantrucco, G., Mariotti, N., and Nicosia, U.: Ammonitico Rosso facies in the framework of the Martani Mountains paleoenvironmental evolution during the Jurassic, in: Rosso Ammonitico Symposium Proceedings, 16–21 June 1980, Rome, edited by: Farinacci, A. and Elmi, S., Edizioni Tecnoscienza, Roma, 311–334, http://pi.lib.uchicago.edu/1001/cat/bib/722066 (last access: 19 Decembver 2024), 1981.
Ferranti, L. and Oldow, J. S.: History and tectonic implications of low-angle detachment faults and orogen parallel extension, Picentini Mountains, Southern Apennines fold and thrust belt, Italy, Tectonics, 18, 498–526, 1999.
Ferranti, L., Oldow, J. S., and Sacchi, M.: Pre-Quaternary orogen-parallel extension in the Southern Apennine belt, Italy, Tectonophysics, 260, 325–347, 1996.
Galadini, F. and Galli, P.: Active tectonics in the Central Apennines (Italy) – input data for seismic hazard assessment, Nat. Hazards, 22, 225–270, 2000.
Galadini, F., Falcucci, E., Galli, P., Giaccio, B., Gori, S., Messina, P., Moro, M., Saroli, M., Scardia, G., and Sposato, A.: Time intervals to assess active and capable faults for engineering practices in Italy, Eng. Geol., 139–140, 50–65, 2012.
Galderisi, A. and Galli, P.: Coulomb stress transfer between parallel faults. The case of Norcia and Mt Vettore normal faults (Italy, 2016 Mw 6.6 earthquake), Results in Geophysical Sciences, 1–4, 100003, https://doi.org/10.1016/j.ringps.2020.100003, 2020.
Galluzzo, F. and Santantonio, M.: The Sabina Plateau: a new element in the Mesozoic palaeogeography of Central Apennines, B. Soc. Geol. Ital., 1, 561–588, 2002.
Gasparini, C., Iannaccone, G., and Scarpa, R.: Fault-plane solutions and seismicity of the Italian peninsula, Tectonophysics, 117, 59–78, 1985.
Hodge, M. S., Venvik, G., Knies, J., van der Lelij, R., Schönenberger, J., Nordgulen, Ø., Brönner, M., Nasuti, A., and Viola, G.: Multiscalar 3D temporal structural characterisation of Smøla island, mid-Norwegian passive margin: an analogue for unravelling the tectonic history of offshore basement highs, Solid Earth, 15, 589–615, https://doi.org/10.5194/se-15-589-2024, 2024.
IAEA: Seismic hazards in site evaluation for nuclear installations, Safety Standards Series No. SSG-9, https://www-pub.iaea.org/MTCD/Publications/PDF/PUB1950_web.pdf (last access: 19 December 2024), 2010.
ISIDe Working Group: Italian Seismological Instrumental and Parametric Database (ISIDe), Istituto Nazionale di Geofisica e Vulcanologia (INGV), https://doi.org/10.13127/ISIDE, 2007.
ITHACA Working Group: ITHACA (ITaly HAzard from CApable faulting), A database of active capable faults of the Italian territory. Version December 2019, ISPRA Geological Survey of Italy, https://sgi.isprambiente.it/ithaca/viewer/index.html (last access: 19 December 2024), 2019.
Kattenhorn, S. A., Aydin, A., Pollard, D. D.: Joints at high angles to normal fault strike: an explanation using 3-D numerical models of fault-perturbed stress fields, J. Struct. Geol., 22, 1–23, 2000.
Keep, M. and McClay, K. R.: Analogue modelling of multiphase rift systems, Tectonophysics, 273, 239–270, 1997.
Keller, J. V. A., Minelli, G., and Pialli, G.: Anatomy of late orogenic extension: The Northern Apennines case, Tectonophysics, 238, 275–294, https://doi.org/10.1016/0040-1951(94)90060-4, 1994.
Laurenzi, M., Stoppa, F., and Villa, I.: Eventi ignei monogenici e depositi piroclastici nel distretto Ultra-Alcalino Umbro-Laziale (ULUD): revisione, aggiornamento e comparazione dei dati cronologici, Plinius, 12, 61–65, 1994.
Lavecchia, G., Boncio, P., Brozzetti, F., Stucchi, M., and Leschiutta, I.: New criteria for seismotectonic zoning in Central Italy: insights from the Umbria–Marche Apennines, Proceedings of the Scientific Meeting `Geological and geodynamic evolution of the Apennines' in memory of Giampaolo Pialli, Foligno (PG), 16–17 February 2000, B. Soc. Geol. Ital., Special Volume 1, 881–890, 2002.
Machette, M. N.: Active, capable, and potentially active faults – a paleoseismic perspective, J. Geodyn., 29, 387–392, 2000.
Malinverno, A. and Ryan, W. B. F.: Extension in the Tyrrhenian sea and shortening in the Apennines as results of arc migration driven by sinking of the lithosphere, Tectonics, 5, 227–245, 1986.
Mantovani, E., Babbucci, D., Tamburelli, C., and Viti, M.: A review on the driving mechanism of the Tyrrhenian-Apennines system: implications for the present seismotectonic setting in the Central-Northern Apennines, Tectonophysics, 476, 22–40, https://doi.org/10.1016/j.tecto.2008.10.032, 2009.
Mariotti, N., Nicosia, U., Pallini, G., and Schiavinotto, F.: Kimmeridgiano recifale presso Case Canepine (M. Martani, Umbria): ipotesi paleogeografiche, Geologica Romana, 18, 295–315, 1979.
Mariucci, M. T. and Montone, P.: IPSI 1.6, Database of Italian Present-day Stress Indicators, Istituto Nazionale di Geofisica e Vulcanologia (INGV), https://doi.org/10.13127/IPSI.1.6, 2024.
Mariucci, M. T., Amato, A., and Montone, P.: Recent tectonic evolution and present stress in the Northern Apennines, Tectonics, 18, 108–118, 1999.
Mattila, J. and Viola, G.: New constraints on 1.7 Gyr of brittle tectonic evolution in southwestern Finland derived from a structural study at the site of a potential nuclear waste repository (Olkiluoto Island), J. Struct. Geol., 67, 50–74, 2014.
McClay, K. R. and White, M. J.: Analogue modelling of orthogonal and oblique rifting, Mar. Petrol. Geol., 12, 137–151, https://doi.org/10.1016/0264-8172(95)92835-K, 1995.
Mercuri, M., Tavani, S., Fabbi, S., Lavosi, G., and Carminati, E.: Long live the fault! Double inversion of a Mesozoic rift-related fault system in the central Apennines, Terra Nova, 36, 358–368, https://doi.org/10.1111/ter.12718, 2024.
Milano, G., Ventura, G., and Di Giovambattista, R.: Seismic evidence of longitudinal extension in the Southern Apennines chain (Italy): the 1997–1998 Sannio–Matese seismic sequence, Geophys. Res. Lett., 29, 65-1–65-4, https://doi.org/10.1029/2002GL015188, 2002.
Milano, G., Di Giovambattista, R., and Ventura, G.: Seismic activity in the transition zone between Southern and Central Apennines (Italy): evidences of longitudinal extension inside the Ortona-Roccamonfina tectonic line, Tectonophysics, 457, 102–110, 2008.
Mildon, Z. K., Roberts, G. P., Faure Walker, J. P., and Iezzi, F.: Coulomb stress transfer and fault interaction over millennia on non-planar active normal faults: the Mw 6.5–5.0 seismic sequence of 2016–2017, central Italy, Geophys. J. Int., 210, 1206–1218, 2017.
Molli, G.: Northern Apennine–Corsica orogenic system: an updated overview, Geological Society of London Special Publication,, 298, 413–442, 2008.
Montone, P., Mariucci, M. T., and Pierdominici, S.: The Italian present-day stress map, Geophys. J. Int., 189, 705–716, https://doi.org/10.1111/j.1365-246X.2012.05391.x, 2012.
Oldow, J. S., D'Argenio, B., Ferranti, L., Pappone, G., Marsella, E., and Sacchi, M.: Largescale longitudinal extension in the southern Apennines contractional belt, Italy, Geology, 21, 1123–1126, 1993.
Pace, P. and Calamita, F.: Push-up inversion structures vs. fault-bend reactivation anticlines along oblique thrust ramps: examples from the Apennines fold-and-thrust belt (Italy), J. Geol. Soc. London, 171, 227–238, https://doi.org/10.1144/jgs2013-053, 2014.
Parotto, M. and Praturlon, A.: Geological summary of the Central Apennines, Quaderni de 'La Ricerca Scientifica', 90, 257–311, 1975.
Patacca, E., Scandone, P., Di Luzio, E., Cavinato, G. P., and Parotto, M.: Structural architecture of the central Apennines: Interpretation of the CROP 11 seismic profile from the Adriatic coast to the orographic divide, Tectonics, 27, TC3006, https://doi.org/10.1029/2005TC001917, 2008.
Piccardi, L., Sani, F., Bonini, M., Boccaletti, M., Moratti, G., and Gualtierotti, A.: Deformazioni quaternarie nell'Appennino centro-settentrionale: evidenze ed implicazioni, Proceedings of the A. I. Q.UA. Congress `Tettonica quaternaria del territorio italiano: conoscenze, problemi ed applicazioni', Parma, 25–27 February 1997, Il Quaternario, 10, 273–280, 1997.
Pizzi, A. and Galadini, F.: Pre-existing cross-structures and active fault segmentation in the northern-central Apennines (Italy), Tectonophysics, 476, 304–319, 2009.
Pondrelli, S., Salimbeni, S., Ekström, G., Morelli, A., Gasperini, P., and Vannucci, G.: The Italian CMT dataset from 1977 to the present, Phys. Earth Planet. In., 159, 286–303, https://doi.org/10.1016/j.pepi.2006.07.008, 2006.
Principi, G. and Treves, B.: Il sistema corso-appenninico come prisma d'accrezione. Riflessi sul problema generale del limite Alpi–Appennini, Memorie della Società Geologica Italiana, 28, 549–576, 1984.
Regione Umbria – Servizio Geologico: Carta geologica dell'Umbria, https://dati.regione.umbria.it/dataset/carta-geologica-dell-umbria (last access: 19 December 2024), 2013.
Roberts, G. P.: Variation in fault-slip directions along active and segmented normal fault systems, J. Struct. Geol., 18, 835–845, 1996.
Rosenbaum, G. and Lister, G. S.: Neogene and Quaternary rollback evolution of theTyrrhenian Sea, the Apennines, and the Sicilian Maghrebides, Tectonics, 23, TC1013, https://doi.org/10.1029/2003TC001518, 2004.
Rosenbaum, G., Lister, G. S., and Duboz, C.: The Mesozoic and Cenozoic motion of Adria (central Mediterranean): constraints and limitations, Geodin. Acta, 17, 125–139, 2004.
Rovida, A., Locati, M., Camassi, R., Lolli, B., and Gasperini, P.: The Italian earthquake catalogue CPTI15, B. Earthq. Eng., 18, 2953–2984, https://doi.org/10.1007/s10518-020-00818-y, 2020.
Rovida, A., Locati, M., Camassi, R., Lolli, B., Gasperini, P., and Antonucci A.: Catalogo Parametrico dei Terremoti Italiani (CPTI15), versione 4.0, Istituto Nazionale di Geofisica e Vulcanologia (INGV), https://doi.org/10.13127/CPTI/CPTI15.4, 2022.
Sabbatino, M., Tavani, S., Vitale, S., Ogata, K., Corradetti, A., Consorti, L., Arienzo, I., Cipriani, A., and Parente, M.: Forebulge migration in the foreland basin system of the central-southern Apennine fold-thrust belt (Italy): New high-resolution Sr-isotope dating constraints, Basin Res., 33, 2817–2836, 2021.
Salvini, F., Billi, A., and Wise, D. U.: Strike-slip fault-propagation cleavage in carbonate rocks: the Mattinata fault zone, Southern Apennines, Italy, J. Struct. Geol. 21, 1731–1749, 1999.
Santantonio, M.: Facies associations and evolution of pelagic carbonate platform/basin systems: examples from the Italian Jurassic, Sedimentology, 40, 1039–1067, 1993.
Santantonio, M. and Carminati, E.: The Jurassic rifting evolution of the Apennines and Southern Alps (Italy): Parallels and differences, Geol. Soc. Am. Bull., 123, 468–484, 2011.
Santantonio, M., Cipriani, A., Fabbi, S., Citton, P., and Romano, M.: PCP-basin settings in the fossil record: state of the art – Guest editorial, Ital. J. Geosci., 139, 5–7, 2020.
Scheiber, T. and Viola, G.: Complex Bedrock Fracture Patterns: A Multipronged Approach to Resolve Their Evolution in Space and Time, Tectonics, 37, 1030–1062, https://doi.org/10.1002/2017TC004763, 2018.
Scisciani, V.: Styles of positive inversion tectonics in the central Apennines and in the Adriatic foreland: Implications for the evolution of the Apennine chain (Italy), J. Struct. Geol., 31, 1276–1294, https://doi.org/10.1016/j.jsg.2009.02.004, 2009.
Scisciani, V., Agostini, S., Calamita, F., Pace, P., Cilli, A., Giori, I., and Paltrinieri, W.: Positive inversion tectonics in foreland fold-and-thrust belts: A reappraisal of the Umbria–Marche Northern Apennines (Central Italy) by integrating geological and geophysical data, Tectonophysics, 637, 218–237, 2014.
Scognamiglio, L., Tinti, E., and Quintiliani, M.: Time Domain Moment Tensor (TDMT) [Data set], Istituto Nazionale di Geofisica e Vulcanologia (INGV), https://doi.org/10.13127/TDMT, 2006.
Tavani, S., Granado, P., Corradetti, A., Camanni, G., Vignaroli, G., Manatschal, G., Mazzoli, S., Muñoz, J. A., and Parente, M.: Rift inheritance controls the switch from thin-to thick-skinned thrusting and basal décollement re-localization at the subduction-to-collision transition, Geol. Soc. Am. Bull., 133, 2157–2170, 2021.
Tavani, S., Smeraglia, L., Fabbi, S., Aldega, L., Sabbatino, M., Cardello, G. L., Maresca, A., Schirripa Spagnolo, G., Kylander-Clark, A., Billi, A., Bernasconi, S. M., and Carminati, E.: Timing, thrusting mode, and negative inversion along the Circeo thrust, Apennines, Italy: How the accretion-to-Extension transition operated during slab rollback, Tectonics, 42, e2022TC007679, https://doi.org/10.1029/2022TC007679, 2023.
Tavarnelli, E.: The effects of pre-existing normal faults on thrust ramp development: an example from the Northern Apennines, Italy, Geol. Rundsch., 85, 363–371, 1996.
Tavarnelli, E., Butler, R. W. H., Decandia, F. A., Calamita, F., Grasso, M., Alvarez, W., and Renda, P.: Implications of fault reactivation and structural inheritance in the Cenozoic tectonic evolution of Italy, Geology of Italy, 1, 209–222, 2004.
Tavarnelli, E., Scisciani, V., Patruno, S., Calamita, F., Pace, P., and Iacopini, D.: The role of structural inheritance in the evolution of fold-and-thrust belts: insights from the Umbria–Marche Apennines, Italy, in: 250 Million Years of Earth History in Central Italy: Celebrating 25 Years of the Geological Observatory of Coldigioco, edited by: Koeberl, C. and Bice, D. M., Geological Society of America, Boulder, CO, Special Paper no. 542, pp. 191–212. 2019.
Technical Commission on Seismic Microzonation: Land Use Guidelines for Areas with Active and Capable Faults (ACF), Conference of the Italian Regions and Autonomous Provinces, Civil Protection Department, Rome, 1–26, https://www.centromicrozonazionesismica.it/documents/18/GuidelinesForSeismicMicrozonation.pdf (last access: 19 December 2024), 2015.
Tensor Program: Fault-kinematic analysis and tectonic stress tensor inversion, http://damiendelvaux.be/Tensor/WinTensor/win-tensor.html (last access: 19 December 2024), 2024.
Vai, G. B. and Martini, I. P.: Anatomy of an Orogen: The Apennines and Adjacent Mediterranean Basins, Springer, Dordrecht, 633 pp., https://doi.org/10.1007/978-94-015-9829-3, 2001.
Vezzani, L., Festa, A., and Ghisetti, F.: Geology and Tectonic Evolution of the Central-Southern Apennines, Italy, Special paper 469, Geological Society of America, Boulder, CO, USA, https://doi.org/10.1130/2010.2469, 2010.
Viola, G., Venvik Ganerød, G., and Wahlgren, C.-H.: Unravelling 1.5 Gyr of brittle deformation history in the Laxemar-Simpevarp area, SE Sweden: a contribution to the Swedish site investigation study for the disposal of highly radioactive nuclear waste, Tectonics, 28, TC5007, https://doi.org/10.1029/2009TC002461, 2009.
Viola, G., Kounov, A., Andreoli, M. A. G., amd Mattila, J.: Brittle tectonic evolution along the western margin of South Africa: more than 500 Myr of continued reactivation, Tectonophysics, 514–517, 93–114, 2012.
Viola, G., Musumeci, G., Mazzarini, F., Tavazzani, L., Curzi, M., Torgersen, E., van der Lelij, R., and Aldega, L.: Structural characterization and K–Ar illite dating of reactivated, complex and heterogeneous fault zones: lessons from the Zuccale Fault, Northern Apennines, Solid Earth, 13, 1327–1351, https://doi.org/10.5194/se-13-1327-2022, 2022.
Wang, L., Maestrelli, D., Corti, G., Zou, Y., and Shen, C.: Normal fault reactivation during multiphase extension: analogue models and application to the Turkana depression, East Africa, Tectonophysics, 811, 228870, https://doi.org/10.1016/j.tecto.2021.228870, 2021.
Wells, D. L. and Coppersmith, K. J.: Empirical relationships among magnitude, rupture length, rupture area, and surface displacement, B. Seismol. Soc. Am., 84, 974–1002, https://doi.org/10.1785/BSSA0840040974, 1994.
Ziegler, P. A.: Evolution of the Arctic-North Atlantic and the Western Tethys, AAPG Memoir., 43, 1–198, 1988.
Zuccari, C., Viola, G., Curzi, M., Aldega, L., and Vignaroli, G.: What steers the “folding to faulting” transition in carbonate-dominated seismic fold-and-thrust belts? New insights from the Eastern Southern Alps (Northern Italy), J. Struct. Geol., 157, 104560, https://doi.org/10.1016/j.jsg.2022.104560, 2022.
Short summary
This study addresses the tectonic evolution of the seismogenic Monti Martani Fault System (northern Apennines, Italy). By applying a field-based structural geology approach, we reconstruct the evolution of the stress field and we challenge the current interpretation of the fault system in terms of both geometry and state of activity. We stress that the peculiar behavior of this system during post-orogenic extension is still significantly influenced by the pre-orogenic structural template.
This study addresses the tectonic evolution of the seismogenic Monti Martani Fault System...
