Articles | Volume 5, issue 2
https://doi.org/10.5194/se-5-611-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-5-611-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
02 Jul 2014
Research article |
| 02 Jul 2014
Did Adria rotate relative to Africa?
D. J. J. van Hinsbergen
Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands
M. Mensink
Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands
C. G. Langereis
Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands
M. Maffione
Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands
L. Spalluto
Dipartimento di Scienze della Terra e Geoambientali, UniversitaÌ degli Studi "Aldo Moro" di Bari, Via E. Orabona 4, 70125, Bari, Italy
M. Tropeano
Dipartimento di Scienze della Terra e Geoambientali, UniversitaÌ degli Studi "Aldo Moro" di Bari, Via E. Orabona 4, 70125, Bari, Italy
L. Sabato
Dipartimento di Scienze della Terra e Geoambientali, UniversitaÌ degli Studi "Aldo Moro" di Bari, Via E. Orabona 4, 70125, Bari, Italy
Related authors
Erik van der Wiel, Cedric Thieulot, and Douwe van Hinsbergen
EGUsphere, https://doi.org/10.31223/X56971, https://doi.org/10.31223/X56971, 2023
Short summary
Short summary
Geodynamic models of mantle convection provide a powerful tool to study the structure and composition of the Earth’s mantle. Comparing such models with other datasets is difficult. We explore the use of 'configurational entropy', which allows to quantify mixing in models. The entropy may be used to analyze the mixed state of the mantle as a whole and may also be useful to validate numerical models against anomalies in the mantle that obtained from seismology and geochemistry.
Alexis Plunder, Cédric Thieulot, and Douwe J. J. van Hinsbergen
Solid Earth, 9, 759–776, https://doi.org/10.5194/se-9-759-2018, https://doi.org/10.5194/se-9-759-2018, 2018
Short summary
Short summary
The thermal state of the Earth's crust determines how it reacts to tectonic forces and to fluid flow responsible for ore formation. We hypothesize that the angle between plate motion and convergent boundaries determines the thermal regime of subduction zones (where a plate goes under another one). Computer models and a geological reconstruction of Turkey were used to validate this hypothesis.
This research was done to validate a hypothesis made on the basis of nonquantitative field data.
Derya Gürer, Douwe J. J. van Hinsbergen, Murat Özkaptan, Iverna Creton, Mathijs R. Koymans, Antonio Cascella, and Cornelis G. Langereis
Solid Earth, 9, 295–322, https://doi.org/10.5194/se-9-295-2018, https://doi.org/10.5194/se-9-295-2018, 2018
Short summary
Short summary
Central and Eastern Anatolia (present-day Turkey) accommodated Africa–Eurasia convergence in Cenozoic times. As a result, the region underwent distributed deformation and rotation. We provide a paleomagnetic dataset from sedimentary basins and assess the timing and amount of rotations. The obtained rotation patterns together with known fault zones suggest that south-central Turkey represents a coherently counterclockwise-rotating domain.
Michiel Baatsen, Douwe J. J. van Hinsbergen, Anna S. von der Heydt, Henk A. Dijkstra, Appy Sluijs, Hemmo A. Abels, and Peter K. Bijl
Clim. Past, 12, 1635–1644, https://doi.org/10.5194/cp-12-1635-2016, https://doi.org/10.5194/cp-12-1635-2016, 2016
Short summary
Short summary
One of the major difficulties in modelling palaeoclimate is constricting the boundary conditions, causing significant discrepancies between different studies. Here, a new method is presented to automate much of the process of generating the necessary geographical reconstructions. The latter can be made using various rotational frameworks and topography/bathymetry input, allowing for easy inter-comparisons and the incorporation of the latest insights from geoscientific research.
G. Hoareau, B. Bomou, D. J. J. van Hinsbergen, N. Carry, D. Marquer, Y. Donnadieu, G. Le Hir, B. Vrielynck, and A.-V. Walter-Simonnet
Clim. Past, 11, 1751–1767, https://doi.org/10.5194/cp-11-1751-2015, https://doi.org/10.5194/cp-11-1751-2015, 2015
Short summary
Short summary
The impact of Neo-Tethys closure on early Cenozoic warming has been tested. First, the volume of subducted sediments and the amount of CO2 emitted along the northern Tethys margin has been calculated. Second, corresponding pCO2 have been tested using the GEOCLIM model. Despite high CO2 production, maximum pCO2 values (750ppm) do not reach values inferred from proxies. Other cited sources of excess CO2 such as the NAIP are also below fluxes required by GEOCLIM to fit with proxy data.
Erik van der Wiel, Cedric Thieulot, and Douwe van Hinsbergen
EGUsphere, https://doi.org/10.31223/X56971, https://doi.org/10.31223/X56971, 2023
Short summary
Short summary
Geodynamic models of mantle convection provide a powerful tool to study the structure and composition of the Earth’s mantle. Comparing such models with other datasets is difficult. We explore the use of 'configurational entropy', which allows to quantify mixing in models. The entropy may be used to analyze the mixed state of the mantle as a whole and may also be useful to validate numerical models against anomalies in the mantle that obtained from seismology and geochemistry.
Alexis Plunder, Cédric Thieulot, and Douwe J. J. van Hinsbergen
Solid Earth, 9, 759–776, https://doi.org/10.5194/se-9-759-2018, https://doi.org/10.5194/se-9-759-2018, 2018
Short summary
Short summary
The thermal state of the Earth's crust determines how it reacts to tectonic forces and to fluid flow responsible for ore formation. We hypothesize that the angle between plate motion and convergent boundaries determines the thermal regime of subduction zones (where a plate goes under another one). Computer models and a geological reconstruction of Turkey were used to validate this hypothesis.
This research was done to validate a hypothesis made on the basis of nonquantitative field data.
Derya Gürer, Douwe J. J. van Hinsbergen, Murat Özkaptan, Iverna Creton, Mathijs R. Koymans, Antonio Cascella, and Cornelis G. Langereis
Solid Earth, 9, 295–322, https://doi.org/10.5194/se-9-295-2018, https://doi.org/10.5194/se-9-295-2018, 2018
Short summary
Short summary
Central and Eastern Anatolia (present-day Turkey) accommodated Africa–Eurasia convergence in Cenozoic times. As a result, the region underwent distributed deformation and rotation. We provide a paleomagnetic dataset from sedimentary basins and assess the timing and amount of rotations. The obtained rotation patterns together with known fault zones suggest that south-central Turkey represents a coherently counterclockwise-rotating domain.
Michiel Baatsen, Douwe J. J. van Hinsbergen, Anna S. von der Heydt, Henk A. Dijkstra, Appy Sluijs, Hemmo A. Abels, and Peter K. Bijl
Clim. Past, 12, 1635–1644, https://doi.org/10.5194/cp-12-1635-2016, https://doi.org/10.5194/cp-12-1635-2016, 2016
Short summary
Short summary
One of the major difficulties in modelling palaeoclimate is constricting the boundary conditions, causing significant discrepancies between different studies. Here, a new method is presented to automate much of the process of generating the necessary geographical reconstructions. The latter can be made using various rotational frameworks and topography/bathymetry input, allowing for easy inter-comparisons and the incorporation of the latest insights from geoscientific research.
G. Hoareau, B. Bomou, D. J. J. van Hinsbergen, N. Carry, D. Marquer, Y. Donnadieu, G. Le Hir, B. Vrielynck, and A.-V. Walter-Simonnet
Clim. Past, 11, 1751–1767, https://doi.org/10.5194/cp-11-1751-2015, https://doi.org/10.5194/cp-11-1751-2015, 2015
Short summary
Short summary
The impact of Neo-Tethys closure on early Cenozoic warming has been tested. First, the volume of subducted sediments and the amount of CO2 emitted along the northern Tethys margin has been calculated. Second, corresponding pCO2 have been tested using the GEOCLIM model. Despite high CO2 production, maximum pCO2 values (750ppm) do not reach values inferred from proxies. Other cited sources of excess CO2 such as the NAIP are also below fluxes required by GEOCLIM to fit with proxy data.
Related subject area
Geodynamics
On the impact of true polar wander on heat flux patterns at the core–mantle boundary
The influence of viscous slab rheology on numerical models of subduction
Statistical appraisal of geothermal heat flow observations in the Arctic
Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath
Modeling liquid transport in the Earth's mantle as two-phase flow: effect of an enforced positive porosity on liquid flow and mass conservation
Thrusts control the thermal maturity of accreted sediments
The crustal structure of the Longmenshan fault zone and its implications for seismogenesis: new insight from aeromagnetic and gravity data
Earth's core variability from magnetic and gravity field observations
Quantifying mantle mixing through configurational Entropy
Various lithospheric deformation patterns derived from rheological contrasts between continental terranes: Insights from 2-D numerical simulations
The role of continental lithospheric thermal structure in the evolution of orogenic systems: application to the Himalayan–Tibetan collision zone
Glacial-isostatic-adjustment strain rate–stress paradox in the Western Alps and impact on active faults and seismicity
How a volcanic arc influences back-arc extension: insight from 2D numerical models
Magmatic underplating associated with Proterozoic basin formation: insights from gravity study over the southern margin of Bundelkhand craton, India
The effect of temperature-dependent material properties on simple thermal models of subduction zones
Plume–ridge interactions: ridgeward versus plate-drag plume flow
Transport mechanisms of hydrothermal convection in faulted tight sandstones
A corrected finite-difference scheme for the flexure equation with abrupt changes in coefficient
Influence of heterogeneous thermal conductivity on the long-term evolution of the lower-mantle thermochemical structure: implications for primordial reservoirs
The role of edge-driven convection in the generation ofvolcanism – Part 2: Interaction with mantle plumes, applied to the Canary Islands
The effect of low-viscosity sediments on the dynamics and accretionary style of subduction margins
Thermal non-equilibrium of porous flow in a resting matrix applicable to melt migration: a parametric study
101 geodynamic modelling: how to design, interpret, and communicate numerical studies of the solid Earth
Crustal structure of the Volgo–Uralian subcraton revealed by inverse and forward gravity modelling
On the choice of finite element for applications in geodynamics
A new finite element approach to model microscale strain localization within olivine aggregates
Interpolation of magnetic anomalies over an oceanic ridge region using an equivalent source technique and crust age model constraint
Coupled dynamics and evolution of primordial and recycled heterogeneity in Earth's lower mantle
Buoyancy versus shear forces in building orogenic wedges
Comparing global seismic tomography models using varimax principal component analysis
Magma ascent mechanisms in the transition regime from solitary porosity waves to diapirism
Analytical solution for residual stress and strain preserved in anisotropic inclusion entrapped in an isotropic host
Gravity effect of Alpine slab segments based on geophysical and petrological modelling
The role of edge-driven convection in the generation of volcanism – Part 1: A 2D systematic study
Gravity modeling of the Alpine lithosphere affected by magmatism based on seismic tomography
Timescales of chemical equilibrium between the convecting solid mantle and over- and underlying magma oceans
The preserved plume of the Caribbean Large Igneous Plateau revealed by 3D data-integrative models
Impact of upper mantle convection on lithosphere hyperextension and subsequent horizontally forced subduction initiation
Pragmatic solvers for 3D Stokes and elasticity problems with heterogeneous coefficients: evaluating modern incomplete LDLT preconditioners
Combined numerical and experimental study of microstructure and permeability in porous granular media
Mapping undercover: integrated geoscientific interpretation and 3D modelling of a Proterozoic basin
Monitoring crustal CO2 flow: methods and their applications to the mofettes in West Bohemia
On the self-regulating effect of grain size evolution in mantle convection models: application to thermochemical piles
Deciphering the metamorphic evolution of the Pulo do Lobo metasedimentary domain (SW Iberian Variscides)
The impact of rheological uncertainty on dynamic topography predictions
The effect of effective rock viscosity on 2-D magmatic porosity waves
Density distribution across the Alpine lithosphere constrained by 3-D gravity modelling and relation to seismicity and deformation
Pore-scale permeability prediction for Newtonian and non-Newtonian fluids
3-D crustal density model of the Sea of Marmara
Oblique rifting: the rule, not the exception
Thomas Frasson, Stéphane Labrosse, Henri-Claude Nataf, Nicolas Coltice, and Nicolas Flament
Solid Earth, 15, 617–637, https://doi.org/10.5194/se-15-617-2024, https://doi.org/10.5194/se-15-617-2024, 2024
Short summary
Short summary
Heat flux heterogeneities at the bottom of Earth's mantle play an important role in the dynamic of the underlying core. Here, we study how these heterogeneities are affected by the global rotation of the Earth, called true polar wander (TPW), which has to be considered to relate mantle dynamics with core dynamics. We find that TPW can greatly modify the large scales of heat flux heterogeneities, notably at short timescales. We provide representative maps of these heterogeneities.
Natalie Hummel, Susanne Buiter, and Zoltán Erdős
Solid Earth, 15, 567–587, https://doi.org/10.5194/se-15-567-2024, https://doi.org/10.5194/se-15-567-2024, 2024
Short summary
Short summary
Simulations of subducting tectonic plates often use material properties extrapolated from the behavior of small rock samples in a laboratory to conditions found in the Earth. We explore several typical approaches to simulating these extrapolated material properties and show that they produce very rigid subducting plates with unrealistic dynamics. Our findings imply that subducting plates deform by additional mechanisms that are less commonly implemented in simulations.
Judith Freienstein, Wolfgang Szwillus, Agnes Wansing, and Jörg Ebbing
Solid Earth, 15, 513–533, https://doi.org/10.5194/se-15-513-2024, https://doi.org/10.5194/se-15-513-2024, 2024
Short summary
Short summary
Geothermal heat flow influences ice sheet dynamics, making its investigation important for ice-covered regions. Here we evaluate the sparse measurements for their agreement with regional solid Earth models, as well as with a statistical approach. This shows that some points should be excluded from regional studies. In particular, the NGRIP point, which strongly influences heat flow maps and the distribution of high basal melts, should be statistically considered an outlier.
Veleda A. P. Muller, Pietro Sternai, and Christian Sue
Solid Earth, 15, 387–404, https://doi.org/10.5194/se-15-387-2024, https://doi.org/10.5194/se-15-387-2024, 2024
Short summary
Short summary
Uplift rates up to 40 mm yr−1 are measured by GNSS in the southern Patagonian Icefield, a remainder of the Patagonian Ice Sheet that covered the Andes in the Last Glacial Maximum (LGM) at 26 ka. Using numerical modelling, we estimate an increase of 150 to 200 °C of the asthenospheric temperature due to the slab window under southern Patagonia, and we show that post-glacial rebound, after the long-term LGM and the short-term Little Ice Age (400 a), contributed to the modern uplift rate budget.
Changyeol Lee, Nestor G. Cerpa, Dongwoo Han, and Ikuko Wada
Solid Earth, 15, 23–38, https://doi.org/10.5194/se-15-23-2024, https://doi.org/10.5194/se-15-23-2024, 2024
Short summary
Short summary
Fluids and melts in the mantle are key to the Earth’s evolution. The main driving force for their transport is the compaction of the porous mantle. Numerically, the compaction equations can yield unphysical negative liquid fractions (porosity), and it is necessary to enforce positive porosity. However, the effect of such a treatment on liquid flow and mass conservation has not been quantified. We found that although mass conservation is affected, the liquid pathways are well resolved.
Utsav Mannu, David Fernández-Blanco, Ayumu Miyakawa, Taras Gerya, and Masataka Kinoshita
Solid Earth, 15, 1–21, https://doi.org/10.5194/se-15-1-2024, https://doi.org/10.5194/se-15-1-2024, 2024
Short summary
Short summary
Accretion during subduction, in which one tectonic plate moves under another, forms a wedge where sediments can be transformed into hydrocarbons. We utilised realistic computer models to investigate this and, in particular, how accretion affects mobility in the wedge and found that the evolution of the wedge and the thrusts it develops fundamentally control the thermal maturity of sediments. This can help us better understand the history of subduction and the formation of hydrocarbons in wedges.
Hai Yang, Shengqing Xiong, Qiankun Liu, Fang Li, Zhiye Jia, Xue Yang, Haofei Yan, and Zhaoliang Li
Solid Earth, 14, 1289–1308, https://doi.org/10.5194/se-14-1289-2023, https://doi.org/10.5194/se-14-1289-2023, 2023
Short summary
Short summary
The Wenchuan (Ms 8.0) and Lushan (Ms 7.0) earthquakes show different geodynamic features and form a 40–60 km area void of aftershocks for both earthquakes. The inverse models suggest that the downward-subducted basement of the Sichuan Basin is irregular in shape and heterogeneous in magnetism and density. The different focal mechanisms of the two earthquakes and the genesis of the seismic gap may be closely related to the differential thrusting mechanism caused by basement heterogeneity.
Anita Thea Saraswati, Olivier de Viron, and Mioara Mandea
Solid Earth, 14, 1267–1287, https://doi.org/10.5194/se-14-1267-2023, https://doi.org/10.5194/se-14-1267-2023, 2023
Short summary
Short summary
To understand core dynamics, insight from several possible observables is needed. By applying several separation methods, we show spatiotemporal variabilities in the magnetic and gravity fields related to the core dynamics. A 7-year oscillation is found in all conducted analyses. The results in the magnetic field reflect the core processes and the variabilities in the gravity field exhibit new findings that might be an interesting input to build an enhanced model of the Earth’s core.
Erik van der Wiel, Cedric Thieulot, and Douwe van Hinsbergen
EGUsphere, https://doi.org/10.31223/X56971, https://doi.org/10.31223/X56971, 2023
Short summary
Short summary
Geodynamic models of mantle convection provide a powerful tool to study the structure and composition of the Earth’s mantle. Comparing such models with other datasets is difficult. We explore the use of 'configurational entropy', which allows to quantify mixing in models. The entropy may be used to analyze the mixed state of the mantle as a whole and may also be useful to validate numerical models against anomalies in the mantle that obtained from seismology and geochemistry.
Renxian Xie, Lin Chen, Jason P. Morgan, and Yonghsun John Chen
EGUsphere, https://doi.org/10.5194/egusphere-2023-2736, https://doi.org/10.5194/egusphere-2023-2736, 2023
Short summary
Short summary
Continental terranes have various rheological strengths due to the differences on their ages, compositions and structures. We applied four assumed rheological models to three terranes in a collisional model, and obtained four styles of lithosphere deformation pattern of collision, subduction, thickening/delamination, and replacement. These simulation patterns are seen in observed lithosphere deformation patterns and structures in East Asia.
Mengxue Liu, Dinghui Yang, and Rui Qi
Solid Earth, 14, 1155–1168, https://doi.org/10.5194/se-14-1155-2023, https://doi.org/10.5194/se-14-1155-2023, 2023
Short summary
Short summary
The continuous subduction mainly occurs with a relatively cold overriding lithosphere (Tmoho ≤ 450 °C), while slab break-off dominates when the model has a relatively hot procontinental Moho temparature (Tmoho ≥ 500 °C). Hr is more prone to facilitating the deformation of the lithospheric upper part than altering the collision mode. The lithospheric thermal structure may have played a significant role in the development of Himalayan–Tibetan orogenic lateral heterogeneity.
Juliette Grosset, Stéphane Mazzotti, and Philippe Vernant
Solid Earth, 14, 1067–1081, https://doi.org/10.5194/se-14-1067-2023, https://doi.org/10.5194/se-14-1067-2023, 2023
Short summary
Short summary
In glaciated regions, induced lithosphere deformation is proposed as a key process contributing to fault activity and seismicity. We study the impact of this effect on fault activity in the Western Alps. We show that the response to the last glaciation explains a major part of the geodetic strain rates but does not drive or promote the observed seismicity. Thus, seismic hazard studies in the Western Alps require detailed modeling of the glacial isostatic adjustment (GIA) transient impact.
Duo Zhang and Huw Davies
EGUsphere, https://doi.org/10.5194/egusphere-2023-1791, https://doi.org/10.5194/egusphere-2023-1791, 2023
Short summary
Short summary
We numerically model the influence of an arc on back-arc extension. The arc is simulated by emplacing a hot region in the overriding plate. We investigate how plate ages and properties of the hot region affect back-arc extension and present regime diagrams of the nature of back-arc extension for these models. We find that back-arc extension not only at the hot region but surprisingly also away from it, and a hot region facilitates extension of the overriding plate.
Ananya P. Mukherjee and Animesh Mandal
EGUsphere, https://doi.org/10.5194/egusphere-2023-1389, https://doi.org/10.5194/egusphere-2023-1389, 2023
Short summary
Short summary
Global gravity data is used to develop 2D models and Moho depth map (from 3D gravity inversion) to depict the crustal structure beneath the region covered by Proterozoic sedimentary basins, south of Bundelkhand craton in central India. The observed thick, mafic underplated layer above Moho points to the existence of Proterozoic plume activity. Thus, the study offers insights into the geodynamic processes that led to the formation the basins thereby about the crustal configuration of this region.
Iris van Zelst, Cedric Thieulot, and Timothy J. Craig
Solid Earth, 14, 683–707, https://doi.org/10.5194/se-14-683-2023, https://doi.org/10.5194/se-14-683-2023, 2023
Short summary
Short summary
A common simplification in subduction zone models is the use of constant thermal parameters, while experiments have shown that they vary with temperature. We test various formulations of temperature-dependent thermal parameters and show that they change the thermal structure of the subducting slab. We recommend that modelling studies of the thermal structure of subduction zones take the temperature dependence of thermal parameters into account, especially when providing insights into seismicity.
Fengping Pang, Jie Liao, Maxim D. Ballmer, and Lun Li
Solid Earth, 14, 353–368, https://doi.org/10.5194/se-14-353-2023, https://doi.org/10.5194/se-14-353-2023, 2023
Short summary
Short summary
Plume–ridge interaction is an intriguing geological process in plate tectonics. In this paper, we address the respective role of ridgeward vs. plate-drag plume flow in 2D thermomechanical models and compare the results with a compilation of observations on Earth. From a geophysical and geochemical analysis of Earth plumes and in combination with the model results, we propose that the absence of plumes interacting with ridges in the Pacific is largely caused by the presence of plate drag.
Guoqiang Yan, Benjamin Busch, Robert Egert, Morteza Esmaeilpour, Kai Stricker, and Thomas Kohl
Solid Earth, 14, 293–310, https://doi.org/10.5194/se-14-293-2023, https://doi.org/10.5194/se-14-293-2023, 2023
Short summary
Short summary
The physical processes leading to the kilometre-scale thermal anomaly in faulted tight sandstones are numerically investigated. The fluid-flow pathways, heat-transfer types and interactions among different convective and advective flow modes are systematically identified. The methodologies and results can be applied to interpret hydrothermal convection-related geological phenomena and to draw implications for future petroleum and geothermal exploration and exploitation in analogous settings.
David Hindle and Olivier Besson
Solid Earth, 14, 197–212, https://doi.org/10.5194/se-14-197-2023, https://doi.org/10.5194/se-14-197-2023, 2023
Short summary
Short summary
By making a change to the way we solve the flexure equation that describes how the Earth's outer layer bends when it is subjected to loading by ice sheets or mountains, we develop new ways of using an old method from geodynamics. This lets us study the Earth's outer layer by measuring a parameter called the elastic thickness, effectively how stiff and springy the outer layer is when it gets loaded and also how the Earth's outer layer gets broken around its edges and in its interior.
Joshua Martin Guerrero, Frédéric Deschamps, Yang Li, Wen-Pin Hsieh, and Paul James Tackley
Solid Earth, 14, 119–135, https://doi.org/10.5194/se-14-119-2023, https://doi.org/10.5194/se-14-119-2023, 2023
Short summary
Short summary
The mantle thermal conductivity's dependencies on temperature, pressure, and composition are often suppressed in numerical models. We examine the effect of these dependencies on the long-term evolution of lower-mantle thermochemical structure. We propose that depth-dependent conductivities derived from mantle minerals, along with moderate temperature and compositional correction, emulate the Earth's mean lowermost-mantle conductivity values and produce a stable two-pile configuration.
Antonio Manjón-Cabeza Córdoba and Maxim D. Ballmer
Solid Earth, 13, 1585–1605, https://doi.org/10.5194/se-13-1585-2022, https://doi.org/10.5194/se-13-1585-2022, 2022
Short summary
Short summary
The origin of many volcanic archipelagos on the Earth remains uncertain. By using 3D modelling of mantle flow and melting, we investigate the interaction between the convective mantle near the continental–oceanic transition and rising hot plumes. We believe that this phenomenon is the origin behind some archipelagos, in particular the Canary Islands. Analysing our results, we reconcile observations that were previously enigmatic, such as the complex patterns of volcanism in the Canaries.
Adina E. Pusok, Dave R. Stegman, and Madeleine Kerr
Solid Earth, 13, 1455–1473, https://doi.org/10.5194/se-13-1455-2022, https://doi.org/10.5194/se-13-1455-2022, 2022
Short summary
Short summary
Sediments play an important role in global volatile and tectonic cycles, yet their effect on subduction dynamics is poorly resolved. In this study, we investigate how sediment properties influence subduction dynamics and obtain accretionary or erosive-style margins. Results show that even a thin layer of sediments can exert a profound influence on the emergent regional-scale subduction dynamics.
Laure Chevalier and Harro Schmeling
Solid Earth, 13, 1045–1063, https://doi.org/10.5194/se-13-1045-2022, https://doi.org/10.5194/se-13-1045-2022, 2022
Short summary
Short summary
Fluid flow through rock occurs in many geological settings on different scales, at different temperature conditions and with different flow velocities. Fluid is either in local thermal equilibrium with the host rock or not. We explore the parameters of porous flow and give scaling laws. These allow us to decide whether porous flows are in thermal equilibrium or not. Applied to magmatic systems, moving melts in channels or dikes moderately to strongly deviate from thermal equilibrium.
Iris van Zelst, Fabio Crameri, Adina E. Pusok, Anne Glerum, Juliane Dannberg, and Cedric Thieulot
Solid Earth, 13, 583–637, https://doi.org/10.5194/se-13-583-2022, https://doi.org/10.5194/se-13-583-2022, 2022
Short summary
Short summary
Geodynamic modelling provides a powerful tool to investigate processes in the Earth’s crust, mantle, and core that are not directly observable. In this review, we present a comprehensive yet concise overview of the modelling process with an emphasis on best practices. We also highlight synergies with related fields, such as seismology and geology. Hence, this review is the perfect starting point for anyone wishing to (re)gain a solid understanding of geodynamic modelling as a whole.
Igor Ognev, Jörg Ebbing, and Peter Haas
Solid Earth, 13, 431–448, https://doi.org/10.5194/se-13-431-2022, https://doi.org/10.5194/se-13-431-2022, 2022
Short summary
Short summary
We present a new 3D crustal model of Volgo–Uralia, an eastern segment of the East European craton. We built this model by processing the satellite gravity data and using prior crustal thickness estimation from regional seismic studies to constrain the results. The modelling revealed a high-density body on the top of the mantle and otherwise reflected the main known features of the Volgo–Uralian crustal architecture. We plan to use the obtained model for further geothermal analysis of the region.
Cedric Thieulot and Wolfgang Bangerth
Solid Earth, 13, 229–249, https://doi.org/10.5194/se-13-229-2022, https://doi.org/10.5194/se-13-229-2022, 2022
Short summary
Short summary
One of the main numerical methods to solve the mass, momentum, and energy conservation equations in geodynamics is the finite-element method. Four main types of elements have been used in the past decades in hundreds of publications. For the first time we compare results obtained with these four elements on a series of geodynamical benchmarks and applications and draw conclusions as to which are the best ones and which are to be preferably avoided.
Jean Furstoss, Carole Petit, Clément Ganino, Marc Bernacki, and Daniel Pino-Muñoz
Solid Earth, 12, 2369–2385, https://doi.org/10.5194/se-12-2369-2021, https://doi.org/10.5194/se-12-2369-2021, 2021
Short summary
Short summary
In the first part of this article, we present a new methodology that we have developed to model the deformation and the microstructural evolutions of olivine rocks, which make up the main part of the Earth upper mantle. In a second part, using this methodology we show that microstructural features such as small grain sizes and preferential grain orientations can localize strain at the same intensity and can act together to produce an even stronger strain localization.
Duan Li, Jinsong Du, Chao Chen, Qing Liang, and Shida Sun
Solid Earth Discuss., https://doi.org/10.5194/se-2021-117, https://doi.org/10.5194/se-2021-117, 2021
Revised manuscript not accepted
Short summary
Short summary
Oceanic magnetic anomalies are generally carried out using only few survey lines and thus there are many areas with data gaps. Traditional interpolation methods based on the morphological characteristics of data are not suitable for data with large gaps. The use of dual-layer equivalent-source techniques may improve the interpolation of magnetic anomaly fields in areas with sparse data which gives a good consideration to the extension of the magnetic lineation feature.
Anna Johanna Pia Gülcher, Maxim Dionys Ballmer, and Paul James Tackley
Solid Earth, 12, 2087–2107, https://doi.org/10.5194/se-12-2087-2021, https://doi.org/10.5194/se-12-2087-2021, 2021
Short summary
Short summary
The lower mantle extends from 660–2890 km depth, making up > 50 % of the Earth’s volume. Its composition and structure, however, remain poorly understood. In this study, we investigate several hypotheses with computer simulations of mantle convection that include different materials: recycled, dense rocks and ancient, strong rocks. We propose a new integrated style of mantle convection including
piles,
blobs, and
streaksthat agrees with various observations of the deep Earth.
Lorenzo G. Candioti, Thibault Duretz, Evangelos Moulas, and Stefan M. Schmalholz
Solid Earth, 12, 1749–1775, https://doi.org/10.5194/se-12-1749-2021, https://doi.org/10.5194/se-12-1749-2021, 2021
Short summary
Short summary
We quantify the relative importance of forces driving the dynamics of mountain building using two-dimensional computer simulations of long-term coupled lithosphere–upper-mantle deformation. Buoyancy forces can be as high as shear forces induced by far-field plate motion and should be considered when studying the formation of mountain ranges. The strength of rocks flooring the oceans and the density structure of the crust control deep rock cycling and the topographic elevation of orogens.
Olivier de Viron, Michel Van Camp, Alexia Grabkowiak, and Ana M. G. Ferreira
Solid Earth, 12, 1601–1634, https://doi.org/10.5194/se-12-1601-2021, https://doi.org/10.5194/se-12-1601-2021, 2021
Short summary
Short summary
As the travel time of seismic waves depends on the Earth's interior properties, seismic tomography uses it to infer the distribution of velocity anomalies, similarly to what is done in medical tomography. We propose analysing the outputs of those models using varimax principal component analysis, which results in a compressed objective representation of the model, helping analysis and comparison.
Janik Dohmen and Harro Schmeling
Solid Earth, 12, 1549–1561, https://doi.org/10.5194/se-12-1549-2021, https://doi.org/10.5194/se-12-1549-2021, 2021
Short summary
Short summary
In partially molten regions within the Earth, the melt is able to move separately from the surrounding rocks. This allows for the emergence of so-called solitary porosity waves, driven by compaction and decompaction due to the melt with higher buoyancy. Our numerical models can predict whether a partially molten region will ascend dominated by solitary waves or diapirism. Even in diapiris-dominated regions, solitary waves will build up and ascend as a swarm when the ascend time is long enough.
Xin Zhong, Marcin Dabrowski, and Bjørn Jamtveit
Solid Earth, 12, 817–833, https://doi.org/10.5194/se-12-817-2021, https://doi.org/10.5194/se-12-817-2021, 2021
Short summary
Short summary
Elastic thermobarometry is an useful tool to recover paleo-pressure and temperature. Here, we provide an analytical model based on the Eshelby solution to calculate the residual stress and strain preserved in a mineral inclusion exhumed from depth. The method applies to ellipsoidal, anisotropic inclusions in infinite isotropic hosts. A finite-element method is also used for a facet effect. Volumetrically averaged stress is shown to be a good proxy for the overall heterogeneous stress stage.
Maximilian Lowe, Jörg Ebbing, Amr El-Sharkawy, and Thomas Meier
Solid Earth, 12, 691–711, https://doi.org/10.5194/se-12-691-2021, https://doi.org/10.5194/se-12-691-2021, 2021
Short summary
Short summary
This study estimates the gravitational contribution from subcrustal density heterogeneities interpreted as subducting lithosphere beneath the Alps to the gravity field. We showed that those heterogeneities contribute up to 40 mGal of gravitational signal. Such density variations are often not accounted for in Alpine lithospheric models. We demonstrate that future studies should account for subcrustal density variations to provide a meaningful representation of the complex geodynamic Alpine area.
Antonio Manjón-Cabeza Córdoba and Maxim D. Ballmer
Solid Earth, 12, 613–632, https://doi.org/10.5194/se-12-613-2021, https://doi.org/10.5194/se-12-613-2021, 2021
Short summary
Short summary
The study of intraplate volcanism can inform us about underlying mantle dynamic processes and thermal and/or compositional anomalies. Here, we investigated numerical models of mantle flow and melting of edge-driven convection (EDC), a potential origin for intraplate volcanism. Our most important conclusion is that EDC can only produce moderate amounts of mantle melting. By itself, EDC is insufficient to support the formation of voluminous island-building volcanism over several millions of years.
Davide Tadiello and Carla Braitenberg
Solid Earth, 12, 539–561, https://doi.org/10.5194/se-12-539-2021, https://doi.org/10.5194/se-12-539-2021, 2021
Short summary
Short summary
We present an innovative approach to estimate a lithosphere density distribution model based on seismic tomography and gravity data. In the studied area, the model shows that magmatic events have increased density in the middle to lower crust, which explains the observed positive gravity anomaly. We interpret the densification through crustal intrusion and magmatic underplating. The proposed method has been tested in the Alps but can be applied to other geological contexts.
Daniela Paz Bolrão, Maxim D. Ballmer, Adrien Morison, Antoine B. Rozel, Patrick Sanan, Stéphane Labrosse, and Paul J. Tackley
Solid Earth, 12, 421–437, https://doi.org/10.5194/se-12-421-2021, https://doi.org/10.5194/se-12-421-2021, 2021
Short summary
Short summary
We use numerical models to investigate the thermo-chemical evolution of a solid mantle during a magma ocean stage. When applied to the Earth, our study shows that the solid mantle and a magma ocean tend toward chemical equilibration before crystallisation of this magma ocean. Our findings suggest that a very strong chemical stratification of the solid mantle is unlikely to occur (as predicted by previous studies), which may explain why the Earth’s mantle is rather homogeneous in composition.
Ángela María Gómez-García, Eline Le Breton, Magdalena Scheck-Wenderoth, Gaspar Monsalve, and Denis Anikiev
Solid Earth, 12, 275–298, https://doi.org/10.5194/se-12-275-2021, https://doi.org/10.5194/se-12-275-2021, 2021
Short summary
Short summary
The Earth’s crust beneath the Caribbean Sea formed at about 90 Ma due to large magmatic activity of a mantle plume, which brought molten material up from the deep Earth. By integrating diverse geophysical datasets, we image for the first time two fossil magmatic conduits beneath the Caribbean. The location of these conduits at 90 Ma does not correspond with the present-day Galápagos plume. Either this mantle plume migrated in time or these conduits were formed above another unknown plume.
Lorenzo G. Candioti, Stefan M. Schmalholz, and Thibault Duretz
Solid Earth, 11, 2327–2357, https://doi.org/10.5194/se-11-2327-2020, https://doi.org/10.5194/se-11-2327-2020, 2020
Short summary
Short summary
With computer simulations, we study the interplay between thermo-mechanical processes in the lithosphere and the underlying upper mantle during a long-term (> 100 Myr) tectonic cycle of extension–cooling–convergence. The intensity of mantle convection is important for (i) subduction initiation, (ii) the development of single- or double-slab subduction zones, and (iii) the forces necessary to initiate subduction. Our models are applicable to the opening and closure of the western Alpine Tethys.
Patrick Sanan, Dave A. May, Matthias Bollhöfer, and Olaf Schenk
Solid Earth, 11, 2031–2045, https://doi.org/10.5194/se-11-2031-2020, https://doi.org/10.5194/se-11-2031-2020, 2020
Short summary
Short summary
Mantle and lithospheric dynamics, elasticity, subsurface flow, and other fields involve solving indefinite linear systems. Tools include direct solvers (robust, easy to use, expensive) and advanced iterative solvers (complex, problem-sensitive). We show that a third option, ILDL preconditioners, requires less memory than direct solvers but is easy to use, as applied to 3D problems with parameter jumps. With included software, we hope to allow researchers to solve previously infeasible problems.
Philipp Eichheimer, Marcel Thielmann, Wakana Fujita, Gregor J. Golabek, Michihiko Nakamura, Satoshi Okumura, Takayuki Nakatani, and Maximilian O. Kottwitz
Solid Earth, 11, 1079–1095, https://doi.org/10.5194/se-11-1079-2020, https://doi.org/10.5194/se-11-1079-2020, 2020
Short summary
Short summary
To describe permeability, a key parameter controlling fluid flows in the Earth’s subsurface, an accurate determination of permeability on the pore scale is necessary. For this reason, we sinter artificial glass bead samples with various
porosities, determining the microstructure and permeability using both
experimental and numerical approaches. Based on this we provide
parameterizations of permeability, which can be used as input parameters for
large-scale numerical models.
Mark D. Lindsay, Sandra Occhipinti, Crystal Laflamme, Alan Aitken, and Lara Ramos
Solid Earth, 11, 1053–1077, https://doi.org/10.5194/se-11-1053-2020, https://doi.org/10.5194/se-11-1053-2020, 2020
Short summary
Short summary
Integrated interpretation of multiple datasets is a key skill required for better understanding the composition and configuration of the Earth's crust. Geophysical and 3D geological modelling are used here to aid the interpretation process in investigating anomalous and cryptic geophysical signatures which suggest a more complex structure and history of a Palaeoproterozoic basin in Western Australia.
Tomáš Fischer, Josef Vlček, and Martin Lanzendörfer
Solid Earth, 11, 983–998, https://doi.org/10.5194/se-11-983-2020, https://doi.org/10.5194/se-11-983-2020, 2020
Short summary
Short summary
Data on CO2 degassing help understanding the relations of the gas flow on geodynamic processes. Long-term gas flow measurements in rough field conditions present a challenge due to technical problems. We describe methods used for CO2 flow monitoring in West-Bohemia/Vogtland, which is typical for high CO2 flow, and present a new robust method based on pressure measurements in a water column. The results of 10 years of CO2 flow measurements and their relation to seismic activity are discussed.
Jana Schierjott, Antoine Rozel, and Paul Tackley
Solid Earth, 11, 959–982, https://doi.org/10.5194/se-11-959-2020, https://doi.org/10.5194/se-11-959-2020, 2020
Short summary
Short summary
We investigate the size of mineral grains of Earth's rocks in computer models of the whole Earth. This is relevant because grain size affects the stiffness (large grains are stiffer) and deformation of the Earth's mantle. We see that mineral grains grow inside stable non-deforming regions of the Earth. However, these regions are less stiff than expected. On the other hand, we find that grain size diminishes during deformation events such as when surface material comes down into the Earth.
Irene Pérez-Cáceres, David Jesús Martínez Poyatos, Olivier Vidal, Olivier Beyssac, Fernando Nieto, José Fernando Simancas, Antonio Azor, and Franck Bourdelle
Solid Earth, 11, 469–488, https://doi.org/10.5194/se-11-469-2020, https://doi.org/10.5194/se-11-469-2020, 2020
Short summary
Short summary
The metamorphism of the Pulo do Lobo unit (SW Iberian Massif) is described in this paper. To this end, three different and complementary methodologies have been applied. The new results reported here contribute to the knowledge of the metamorphic conditions of the Pulo do Lobo unit in relation to its deformation. Furthermore, the results are compared in order to assess the reliability of the different methods applied.
Ömer F. Bodur and Patrice F. Rey
Solid Earth, 10, 2167–2178, https://doi.org/10.5194/se-10-2167-2019, https://doi.org/10.5194/se-10-2167-2019, 2019
Short summary
Short summary
Convection in the deep Earth dynamically changes the elevation of plates. Amplitudes of those vertical motions predicted from numerical models are significantly higher than observations. We find that at small wavelengths (< 1000 km) this misfit can be due to the oversimplification in viscosity of rocks. By a suite of numerical experiments, we show that considering the non–Newtonian rheology of the mantle results in predictions in amplitude of dynamic topography consistent with observations.
Janik Dohmen, Harro Schmeling, and Jan Philipp Kruse
Solid Earth, 10, 2103–2113, https://doi.org/10.5194/se-10-2103-2019, https://doi.org/10.5194/se-10-2103-2019, 2019
Short summary
Short summary
In source regions of magmatic systems the temperature is above solidus and melt ascent is assumed to occur predominantly by two-phase flow. This two-phase flow allows for the emergence of solitary porosity waves. By now most solutions of these waves used strongly simplified viscosity laws, while in our laws the viscosity decreases rapidly for small melt fractions. The results show that for higher background porosities the phase velocities and the width of the wave are significantly decreased.
Cameron Spooner, Magdalena Scheck-Wenderoth, Hans-Jürgen Götze, Jörg Ebbing, György Hetényi, and the AlpArray Working Group
Solid Earth, 10, 2073–2088, https://doi.org/10.5194/se-10-2073-2019, https://doi.org/10.5194/se-10-2073-2019, 2019
Short summary
Short summary
By utilising both the observed gravity field of the Alps and their forelands and indications from deep seismic surveys, we were able to produce a 3-D structural model of the region that indicates the distribution of densities within the lithosphere. We found that the present-day Adriatic crust is both thinner and denser than the European crust and that the properties of Alpine crust are strongly linked to their provenance.
Philipp Eichheimer, Marcel Thielmann, Anton Popov, Gregor J. Golabek, Wakana Fujita, Maximilian O. Kottwitz, and Boris J. P. Kaus
Solid Earth, 10, 1717–1731, https://doi.org/10.5194/se-10-1717-2019, https://doi.org/10.5194/se-10-1717-2019, 2019
Short summary
Short summary
Prediction of rock permeability is of crucial importance for several research areas in geoscience. In this study, we enhance the finite difference code LaMEM to compute fluid flow on the pore scale using Newtonian and non-Newtonian rheologies. The accuracy of the code is demonstrated using several analytical solutions as well as experimental data. Our results show good agreement with analytical solutions and recent numerical studies.
Ershad Gholamrezaie, Magdalena Scheck-Wenderoth, Judith Bott, Oliver Heidbach, and Manfred R. Strecker
Solid Earth, 10, 785–807, https://doi.org/10.5194/se-10-785-2019, https://doi.org/10.5194/se-10-785-2019, 2019
Short summary
Short summary
Based on geophysical data integration and 3-D gravity modeling, we show that significant density heterogeneities are expressed as two large high-density bodies in the crust below the Sea of Marmara. The location of these bodies correlates spatially with the bends of the main Marmara fault, indicating that rheological contrasts in the crust may influence the fault kinematics. Our findings may have implications for seismic hazard and risk assessments in the Marmara region.
Sascha Brune, Simon E. Williams, and R. Dietmar Müller
Solid Earth, 9, 1187–1206, https://doi.org/10.5194/se-9-1187-2018, https://doi.org/10.5194/se-9-1187-2018, 2018
Short summary
Short summary
Fragmentation of continents often involves obliquely rifting segments that feature a complex three-dimensional structural evolution. Here we show that more than ~ 70 % of Earth’s rifted margins exceeded an obliquity of 20° demonstrating that oblique rifting should be considered the rule, not the exception. This highlights the importance of three-dimensional approaches in modelling, surveying, and interpretation of those rift segments where oblique rifting is the dominant mode of deformation.
Cited articles
Agnini, C., Muttoni, G., Kent, D. V., and Rio, D.: Eocene biostratigraphy and magnetic stratigraphy from Possagno, Italy: The calcareous nannofossil response to climate variability, Earth Planet. Sci. Lett., 241, 815–830, 2006.
Agnini, C., Fornaciari, E., Giusberti, L., Grandesso, P., Lanci, L., Luciani, V., Muttoni, G., Pälike, H., Rio., D., Spofforth, D. J. A., and Stefani, C.: Integrated biomagnetostratigraphy of the Alano section (NE Italy): A proposal for defining the middle-late Eocene boundary, Geol. Soc. Am. Bull., 123, 841–872, 2011.
André, P. and Doulcet, A.: Rospo mare field – Italy, Apulian Platform, Adriatic Sea, in: "Treatise of Petroleum Geology, Atlas of Oil and Gas Fields, Stratigraphic Traps II", edited by: Foster, N. H. and Beaumont, E. A., AAPG, Tulsa, 29–54, 1991.
Argnani, A.: The strait of sicily rift zone: Foreland deformation related to the evolution of a back-arc basin, J. Geodynam., 12, 311–331, 1990.
Argnani, A.: Evolution of the southern Tyrrhenian slab tear and active tectonics along the western edge of the Tyrrhenian subducted slab, Geological Society, London, Special Publications, 311, 193–212, 2009.
Argnani, A.: The influence of Mesozoic Palaeogeography on the variations in structural style along the front of the Albanide thrust-and-fold belt, IJG, 132, 175–185, 2013.
Argnani, A. and Bonazzi, C.: Malta Escarpment fault zone offshore eastern Sicily: Pliocene-Quaternary tectonic evolution based on new multichannel seismic data, Tectonics, 24, TC4009, https://doi.org/10.1029/2004TC001656, 2005.
Argnani, A., Marina, I. G., CNR, B., Favali, P., Frugoni, F., Gasperini, M., Ligi, M., Marani, M., and Mele, G.: Tettonica dell'Adriatico meridionale, Mem. Soc. Geol. It., 51, 227–237, 1996.
Argnani, A., Frugoni, F., Cosi, R., Ligi, M., and Favali, P.: Tectonics and seismicity of the Apulian Ridge south of Salento peninsula (Southern Italy), Ann. Geophys., 44, 527–540, 2001.
Belguith, Y., Geoffroy, L., Mourgues, R., and Rigane, A.: Analogue modelling of Late Miocene–Early Quaternary continental crustal extension in the Tunisia–Sicily Channel area, Tectonophysics, 608, 576–585, 2013.
Bernoulli, D. and Jenkyns, H. C.: Ancient oceans and continental margins of the Alpine- Mediterranean Tethys: deciphering clues from Mesozoic pelagic sediments and ophiolites, Sedimentology, 56, 149–190, 2009.
Bertotti, G., Picotti, V., Chilovi, C., Fantoni, R., Merlini, S., and Mosconi, A.: Neogene to Quaternary sedimentary basins in the south Adriatic (Central Mediterranean): foredeeps and lithospheric buckling, Tectonics, 20, 771–787, 2001.
Bonardi, G., Amore, F. O., Ciampo, G., and de Capoa, P.: Complesso Liguride Auct.: stato delle conoscenze e problemi aperti sulla sua evoluzione pre-appenninica ed i suoi rapporti con l'Arco Calabro, Memorie della Societa Geologica Italiana, 41, 17–35, 1988.
Bosellini, A.: Dinosaurs "re-write" the geodynamics of the eastern Mediterranean and the paleogeography of the Apulia Platform, Earth Sci. Rev., 59, 211–234, 2002.
Bosellini, A., Bosellini, F. R., Colalongo, M. L., Parente, M., Russo, A., and Vescogni, A.: Statigraphic architecture of the Salento coast from Capo d'Otranto to S. Maria di Leuca (Apulia, southern Italy), Rivista Italiana di Paleontologia e Stratigrafia, 105, 397–416, 1999a.
Bosellini, A., Morsilli, M., and Neri, C.: Long-term event stratigraphy of the Apulia Platform margin (Upper Jurassic to Eocene, Gargano, southern Italy), J. Sed. Res., 69, 1241–1252, 1999b.
Bosellini, F. R.: Biotic changes and their control on Oligocene-Miocene reefs: A case study from the Apulia Platform margin (southern Italy), Palaeogeogr. Palaeocl., 241, 393–409, 2006.
Bosellini, F. R. and Russo, A.: Stratigraphy and facies of an Oligocene fringing reef (Castro Limestone, Salento Peninsula, southern Italy), Facies, 26, 145–165, 1992.
Bosellini, F. R., Russo, A., and Vescogni, A.: Messinian reef-building assemblages of the Salento Peninsula (southern Italy): palaeobathymetric and palaeoclimatic significance, Palaeogeogr. Palaeocl., 175, 7–26, 2001.
Butler, R. F.: Paleomagnetism: Magnetic Domains to Geologic Terranes, Blackwell Scientific Publications, Boston. 1992.
Capitanio, F. A. and Goes, S.: Mesozoic spreading kinematics: consequences for Cenozoic Central and Western Mediterranean subduction, Geophys. J. Internat., 165, 804–816, 2006.
Capitanio, F. A., Faccenna, C., Funiciello, R., and Salvini, F.: Recent tectonics of Tripolitania, Libya: an intraplate record of Mediterranean subduction, Geological Society, London, Special Publications, 357, 319–328, 2011.
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.
Catalano, R., Doglioni, C., and Merlini, S.: On the mesozoic Ionian basin, Geophys. J. Internat., 144, 49–64, 2001.
Cavazza, W., Ziegler, P. A., Spakman, W., and Stampfi, G.: The TRANSMED Atlas, Heidelberg, 1–127, 2004.
Chamot-Rooke, N. and Rangin, C.: DOTMED–-Deep Offshore Tectonics of the Mediterranean: A synthesis of deep marine data in eastern Mediterranean, Mem. Soc. Geol. Fr, 177, 1–64, 2005.
Channell, J.: Palaeomagnetism of limestones from the Gargano Peninsula (Italy), and the implication of these data, Geophys. J. Roy. Astronom. Soc., 51, 605–616, 1977.
Channell, J. and Tarling, D. H.: Palaeomagnetism and the rotation of Italy, Earth Planet. Sci. Lett., 25, 177–188, 1975.
Channell, J., D'Argenio, B., and Horvath, F.: Adria, the African promontory, in Mesozoic Mediterranean palaeogeography, Earth Sci. Rev., 15, 213–292, 1979.
Channell, J. E. T.: Palaeomagnetism and palaeogeography of Adria, Geological Society, London, Special Publications, 105, 119–132, 1996.
Channell, J. E. T., Casellato, C. E., Muttoni, G., and Erba, E.: Magnetostratigraphy, nannofossil stratigraphy and apparent polar wander for Adria-Africa in the Jurassic – Cretaceous boundary interval, Palaeogeogr. Palaeocl., 293, 51–75, 2010.
Ciaranfi, N., Pieri, P., and Ricchetti, G.: Note alla carta geologica delle Murge, Mem. Soc. Geol. It., 41, 449–460, 1988.
Cifelli, F., Mattei, M., and Rossetti, F.: Tectonic evolution of arcuate mountain belts on top of a retreating subduction slab: The example of the Calabrian Arc, J. Geophys. Res., 112, B09101, https://doi.org/10.1029/2006JB004848, 2007.
Civile, D., Lodolo, E., Tortorici, L., Lanzafame, G., and Brancolini, G.: Relationships between magmatism and tectonics in a continental rift: The Pantelleria Island region (Sicily Channel, Italy), Mar. Geol., 251, 32–46, 2008.
Civile, D., Lodolo, E., Accettella, D., and Geletti, R.: The Pantelleria graben (Sicily Channel, central Mediterranean): an example of intraplate "passive"rift, Tectonophysics, 490, 174–183, 2010.
Creer, K. M., Irving, A. J., and Nairn, A. E. M.: Paleomagnetism of the Great Whin Sill, Geophys. J. Roy. Astronom. Soc., 2, 306–323, 1959.
D'Agostino, N., Avallone, A., Cheloni, D., D'Anastasio, E., Mantenuto, S., and Selvaggi, G.: Active tectonics of the Adriatic region from GPS and earthquake slip vectors, J. Geophys. Res., 113, B12413, https://doi.org/10.1029/2008JB005860, 2008.
Dallanave, E., Agnini, C., Muttoni, G.. and Rio, D.: Magneto-biostratigraphy of the Cicogna section (Italy): Implications for the late Paleocene–early Eocene time scale, Earth Planet. Sci. Lett., 285, 39–51, 2009.
Dallanave, E., Agnini, C., Muttoni, G., and Rio, D.: Paleocene magneto- biostratigraphy and climate-controlled rock magnetism from the Belluno Basin, Tethys Ocean, Italy, Palaeogeogr. Palaeocl., 337/338, 130–142, 2012.
D'Argenio, B., Pescatore, T.. and Scandone, P.: Schema geologico dell'Appennino meridionale (Campania e Lucania), Accademia Nazionale dei Lincei, 183, 49–72, 1973.
de Alteriis, G.: Different foreland basins in Italy: examples from the central and southern Adriatic Sea, Tectonophysics, 252, 349–373, 1995.
Deenen, M. H. L., Langereis, C. G., van Hinsbergen, D. J. J., and Biggin, A. J.: Geomagnetic secular variation and the statistics of palaeomagnetic directions, Geophys. J. Internat., 186, 509–520, 2011.
Del Ben, A., Geletti, R., and Mocnik, A.: Relation between recent tectonics and inherited Mesozoic structures of the central-southern Adria plate, Bollettino di Geofisica Teoretica ed Applicata, 51, 99–115, 2010.
Dercourt, J., Zonenshain, L.P., Ricou, L. E., and Kazmin, V. G.: Geological evolution of the Tethys belt from the Atlantic to the Pamirs since the Lias, Tectonophysics, 123, 241–315, 1986.
Dewey, J. F., Helman, M. L., Knott, S. D., Turco, E., and Hutton, D. H. W.: Kinematics of the western Mediterranean, Geological Society, London, Special Publications, 45, 265–283, 1989.
Doglioni, C.: A proposal for the kinematic modelling of W-dipping subductions – possible applications to the Tyrrhenian-Apennines system, Terra Nova, 3, 423–434, 1991.
Doglioni, C., Mongelli, F., and Pieri, P.: The Puglia uplift (SE Italy): An anomaly in the foreland of the Apenninic subduction due to buckling of a thick continental lithosphere, Tectonics, 13, 1309–1321, 1994.
Doglioni, C., Gueguen, E., Sabàt, F., and Fernandez, M.: The Western Mediterranean extensional basins and the Alpine orogen, Terra Nova 9, 109–112, 1997.
Faccenna, C. and Becker, T. W.: Shaping mobile belts by small-scale convection, Nature, 465, 602–605, 2010.
Faccenna, C., Funiciello, F., Giardini, D., and Lucente, P.: Episodic back-arc extension during restricted mantle convection in the Central Mediterranean, Earth Planet. Sc. Lett., 187, 105–116, 2001.
Faccenna, C., Piromallo, C., Crespo-Blanc, A., Jolivet, L., and Rossetti, F.: Lateral slab deformation and the origin of the western Mediterranean arcs, Tectonics, 23, TC1012 https://doi.org/10.1029.2002TC001488, 2004.
Fantoni, R. and Franciosi, R.: Tectono-sedimentary setting of the Po Plain and Adriatic foreland, Rend. Fis. Acc. Lincei, 21, 197–209, 2010.
Favali, P., Mele, G., and Mattietti, G.: Contribution to the study of the Apulian microplate geodynamics, Mem. Soc. Geol. It., 44, 71–80, 1990.
Favali, P., Funiciello, R., Mattietti, G., Mele, G., and Salvini, F.: An active margin across the Adriatic Sea (central Mediterranean Sea), Tectonophysics, 219, 109–117, 1993.
Favre, P. and Stampfli, G. M.: From rifting to passive margin: the examples of the Red Sea, Central Atlantic and Alpine Tethys, Tectonophysics, 215, 69–97, 1992.
Festa, V.: Cretaceous structural features of the Murge area (Apulian Foreland, Southern Italy), Eclogae Geol. Helv., 96, 11–22, 2003.
Festa, V., Tropeano, M., and Sabato, L.: New insights on diapirism in the Adriatic Sea: the Tremiti salt structure (Apulia offshore, southeastern Italy), Terra Nova, 26, 169–178, 2014.
Finetti, I.: Structure, stratigraphy and evolution of the central Mediterranean Sea, Bolletino di Geofisica Teoretica ed Applicata, 24, 247–312, 1982.
Finetti, I.: Structure and Evolution of the Central Mediterranean (Pelagian and Ionian Seas), Springer New York, New York, NY, 215–230, 1985.
Fisher, R. A.: Dispersion on a sphere, Proc. Roy. Soc. Lond., A217, 295–305, 1953.
Flores, G., Pieri, M., and Sestini, G.: Geodynamic history and petroleum habitats of the south-east Adriatic region, AAPG Special Publication, 1, 389–398, 1991.
Frisch, W.: Tectonic progradation and plate tectonic evolution of the Alps, Tectonophysics, 60, 121–139, 1979.
Frizon de Lamotte, D., Raulin, C., Mouchot, N., Wrobel-Daveau, J.-C., Blanpied, C., and Ringenbach, J.-C.: The southernmost margin of the Tethys realm during the Mesozoic and Cenozoic: Initial geometry and timing of the inversion processes, Tectonics, 30, TC3002, https://doi.org/10.1029.2010TC002691, 2011.
Gaina, C., Roest, W. R., and Müller, R. D.: Late Cretaceous-Cenozoic deformation of northeast Asia, Earth Planet. Sci. Lett., 197, 273–286, 2002.
Gaina, C., Torsvik, T. H., van Hinsbergen, D. J. J., Medvedev, S., Werner, S. C., and Labails, C.: The African Plate: A history of oceanic crust accretion and subduction since the Jurassic, Tectonophysics, 604, 4–25, 2013.
Gallais, F., Gutscher, M.-A., Graindorge, D., Chamot-Rooke, N., and Klaeschen, D.: A Miocene tectonic inversion in the Ionian Sea (central Mediterranean): Evidence from multichannel seismic data, J. Geophys. Res., 116, B12108, https://doi.org/10.1029.2011JB008505, 2011.
Gambini, R. and Tozzi, M.: Tertiary geodynamic evolution of the Southern Adria microplate, Terra Nova, 8, 593–602, 1996.
Goes, S., Giardini, D., Jenny, S., Hollenstein, C., Kahle, H. G., and Geiger, A.: A recent tectonic reorganization in the south-central Mediterranean, Earth Planet. Sci. Lett., 226, 335–345, 2004.
Golonka, J.: Plate tectonic evolution of the southern margin of Eurasia in the Mesozoic and Cenozoic, Tectonophysics, 381, 235–273, 2004.
Govers, R. and Wortel, M. J. R.: Lithosphere tearing at STEP faults: Response to edges of subduction zones, Earth Planet. Sci. Lett., 236, 505–523, 2005.
Gradstein, F. M., Ogg, J. G., Schmitz, M., and Ogg, G.: The Geologic Time Scale 2012, Elsevier, Amsterdam, 2012.
Grandic, S., Biancone, M., and Samarzija, J.: Geophysical and stratigraphic evidence of the Triassic rift structuration in the Adriatic offshore area, Mem. Soc. Geol. It., 57, 315–325, 2002.
Gueguen, E., Doglioni, C., and Fernandez, M.: On the post-25 Ma geodynamic evolution of the western Mediterranean, Tectonophysics, 298, 259–269, 1998.
Handy, M. R., Schmid, S. M., Bousquet, R., Kissling, E., and Bernoulli, D.: Reconciling plate-tectonic reconstructions of Alpine Tethys with the geological–geophysical record of spreading and subduction in the Alps, Earth Sci. Rev., 102, 121–158, 2010.
Hieke, W., Cita, M. B., and Forcella, F.: Geology of the Victor Hensen Seahill (Ionian Sea, eastern Mediterranean); insights from the study of cored sediment sequences, Boll. Soc. Geol. Italiana, 125, 245–257, 2006.
Iannone, A. and Laviano, A.: Studio stratigrafico e paleoambientale di una successione cenomaniano-turoniana (Calcare di Bari) affiorante presso Ruvo di Puglia, Geologica Romana, 1980.
Johnson, C. L., Constable, C. G., Tauxe, L., Barendregt, R., Brown, L. L., Coe, R. S., Layer, P., Mejia, V., Opdyke, N. D., Singer, B. S., Staudigel, H., and Stone, D. B.: Recent investigations of the 0–5 Ma geomagnetic field recorded by lava flows, Geochem. Geophys. Geosys., 9, Q04032, https://doi.org/10.1029.2007GC001696, 2008.
Jolivet, L., Faccenna, C., and Piromallo, C.: From mantle to crust: Stretching the Mediterranean, Earth Planet. Sci. Lett., 285, 198–209, 2009.
Kastelic, V., Vannoli, P., Burrato, P., Fracassi, U., Tiberti, M. M., and Valensise, G.: Marine and Petroleum Geology, Mar. Petrol. Geol., 42, 191–213, 2013.
Kirschvink, J. L.: The least-squares line and plane and the analysis of palaeomagnetic data, Geophys. J. Roy. Astronom. Soc., 62, 699–718, 1980.
Kokkalas, S., Kamberis, E., Xypolias, P., and Sotiropoulos, S.: Coexistence of thin-and thick-skinned tectonics in Zakynthos area (western Greece): Insights from seismic sections and regional seismicity, Tectonophysics, 597–598, 73–84, 2012.
Laviano, A., Maresca, M. G., and Tropeano, M.: Stratigraphic organization of rudist biogenic beds in the Upper Cenomanian successions of the Western Murge (Apulia, Southern Italy), Geobios, 31, 159–168, 1998.
Luperto-Sinni, E. and Masse, J.-P.: Données nouvelles sur la micropaléontologie et la stratigraphie de la partie basale du "`Calcare di Bari"' (Crétacé inférieur) dans la région des Murges (Italie méridionale), Rivista Italiana di Paleontologia e Stratigrafia, 90, 331–374, 1984.
Malinverno, A. and Ryan, W. B. F.: Extension in the Tyrrhenian Sea and shortening in the Apennines as result of arc migration driven by sinking of the lithosphere, Tectonics, 5, 227–245, 1986.
Márton, E. and Nardi, G.: Cretaceous palaeomagnetic results from Murge (Apulia, southern Italy) : tectonic implications, Geophys. J. Internat., 119, 842–856, 1994.
Márton, E., Drobne, J., \'Cosović, V., and Moro, A.: Palaeomagnetic evidence for Tertiary counterclockwise rotation of Adria, Tectonophysics, 377, 143–156, 2003.
Márton, E., \'Cosović, V., Moro, A. and Zvocak, S.: The motion of Adria during the Late jurassic and Cretacous: New paleomagnetic results from stable Istria, Tectonophysics, 454, 44–53, 2008.
Márton, E., Zampieri, D., Grandesso, P., \'Cosović, V., and Moro, A.: New Cretaceous paleomagnetic results from the foreland of the Southern Alps and the refined apparent polar wander path for stable Adria, Tectonophysics, 480, 57–72, 2010.
Márton, E., Zampieri, D., Kázmér, M., Dunkl, I., and Frisch, W.: New Paleocene–Eocene paleomagnetic results from the foreland of the Southern Alps confirm decoupling of stable Adria from the African plate, Tectonophysics, 504, 89–99, 2011.
Mastrogiacomo, G., Moretti, M., Owen, G., and Spalluto, L.: Tectonic triggering of slump sheets in the Upper Cretaceous carbonate succession of the Porto Selvaggio area (Salento peninsula, southern Italy): Synsedimentary tectonics in the Apulian Carbonate Platform, Sediment. Geol., 269, 15–27, 2012.
Mattavelli, L., Novelli, L., and Anelli, L.: Occurrence of hydrocarbons in the Adriatic basin, AAPG Special Publication, 1, 369–380, 1991.
McFadden and McElhinny, M. W.: Classification of the reversal test in palaeomagnetism, Geophys. J. Internat., 103, 725–729, 1990.
Minelli, L. and Faccenna, C.: Evolution of the Calabrian accretionary wedge (central Mediterranean), Tectonics, 29, TC4004, https://doi.org/10.1029.2009TC002562, 2010.
Mullender, T. A. T., Van Velzen, A. J., and Dekkers, M. J.: Continuous drift correction and separate identification of ferrimagnetic and paramagnetic contribution in thermamagnetic runs, Geophys. J. Internat., 114, 663–672, 1993.
Müller, R. D., Royer, J.-Y., Cande, S. C., Roest, W. R., and Maschenkov, S.: New constraints on the Late Cretaceous/Tertiary plate tectonic evolution of the Caribbean, Sediment. Basins World, 4, 33–59, 1999.
Muttoni, G., Erba, E., Kent, D. V., and Bachtadse, V.: Mesozoic Alpine facies deposition as a result of past latitudinal plate motion, Nature, 434, 59–63, 2005.
Muttoni, G., Dallanave, E., and Channell, J. E. T.: The drift history of Adria and Africa from 280 Ma to Present, Jurassic true polar wander, and zonal climate control on Tethyan sedimentary facies, Palaeogeogr. Palaeocl., 386, 415–435, 2013.
Oldow, J. S., Ferranti, L., D'Argenio, B., Catalano, R., and Pappone, G.: Active fragmentation of Adria, the north African promontory, central Mediterranean orogen, Geology, 30, 779–774, 2002.
Parente, M.: A revised stratigraphy of the Upper Cretaceous to Oligocene units from southeastern Salento (Apulia, southern Italy), Boll. Soc. Paleont. Ital., 33, 155–170, 1994.
Pasquale, V., Verdoya, M., and Chiozzi, P.: Thermal Structure of the Ionian Slab, Pure Appl. Geophys., 162, 967–986, 2005.
Picha, F. J.: Late orogenic strike-slip faulting and escape tectonics in frontal Dinarides-Hellenides, Croatia, Yugoslavia, Albania, and Greece, AAPG Bulletin, 86, 1659–1671, 2002.
Pieri, P. and Laviano, A.: Tettonica e sedimentazione nei depositi senoniani delle Murge sud-orientali (Ostuni), Bollettino della Società Geologica Italiana, 108, 351–356, 1989.
Pieri, P., Festa, V., Moretti, M., and Tropeano, M.: Quaternary tectonic activity of the Murge area (Apulian foreland – Southern Italy), Ann. Geophys., 40, 1395–1404, 1997.
Pomar, L., Mateu-Vicens, G., Morsilli, M., and Brandano, M. : Carbonate ramp evolution during the Late Oligocene (Chattian), Salento Peninsula, southern Italy, Palaeogeogr. Palaeocl., 404, 109–132, 2014.
Reina, A. and Luperto-Sinni, E.: Contributo alla conoscenza stratigrafica del Cretaceo superiore in facies di piattaforma carbonatica interna del Salento occidentale (Puglia, Italia meridionale), Boll. Soc. Geol. Italiana, 33, 145–153, 1994a.
Reina, A. and Luperto-Sinni, E.: Le Dolomie di Monte S. Elia: proposta per una nuova unità formazionale del Cretaceo delle Murge (Puglia, Italia meridionale), Paleopelagos, 4, 233–241, 1994b.
Reston, T. J., Huene, von, R., Dickmann, R., Klaeschen, D., and Kopp, H.: Frontal accretion along the western Mediterranean Ridge: the effect of Messinian evaporites on wedge mechanics and structural style, Mar. Geol., 186, 59–82, 2002.
Ricchetti, G.: Nuovi dati stratigrafici sul Cretaceo delle Murge emersi da indagini nel sottosuolo, Bolletino di Societa Geologica Italiana, 94, 1083–1108, 1975.
Ricchetti, G., Ciaranfi, N., Luperto-Sinni, E., Mongelli, F., and Pieri, P.: Geodinamica ed evoluzione sedimentaria e tettonica dell'avampaese apulo, Mem. Soc. Geol. It., 41, 57–82, 1998.
Robertson, A. H. F., Clift, P. D., Degnan, P. J., and Jones, G.: Palaeogeographic and palaeotectonic evolution of the Eastern Mediterranean Neotethys, Palaeogeogr. Palaeocl., 87, 289–343, 1991.
Rosenbaum, G. and Lister, G. S.: Formation of arcuate orogenic belts in the western Mediterranean region, Orogenic curvature: integrating paleomagnetic and structural analyses, 41–56, 2004.
Rosenbaum, G. and Lister, G. S.: The Western Alps from the Jurassic to Oligocene: spatio-temporal constraints and evolutionary reconstructions, Earth Sci. Rev., 69, 281–306, 2005.
Rosenbaum, G., Lister, G. S., and Duboz, C.: Relative motions of Africa, Iberia and Europe during Alpine orogeny, Tectonophysics, 359, 117–129, 2002.
Rosenbaum, G., Lister, G. S., and Duboz, C.: The Mesozoic and Cenozoic motion of Adria (central Mediterranean): a review of constraints and limitations, Geodinam. Acta, 17, 125–139, 2004.
Rosenbaum, G., Gasparon, M., Lucente, F. P., Peccerillo, A., and Miller, M. S.: Kinematics of slab tear faults during subduction segmentation and implications for Italian magmatism, Tectonics, 27, TC2008, https://doi.org/10.1029.2007TC002143, 2008.
Royden, L. H. and Papanikolaou, D. J.: Slab segmentation and late Cenozoic disruption of the Hellenic arc, Geochem. Geophys. Geosyst., 12, Q03010, https://doi.org/10.1029.2010GC003280, 2011.
Savostin, L. A., Sibuet, J. C., Zonenshain, L.P., Le Pichon, X., and Roulet, M.-J.: Kinematic evolution of the Tethys belt from the Atlantic Ocean to the Pamirs since the Triassic, Tectonophysics, 123, 1–35, 1986.
Scheepers, P.: No tectonic rotation for the Apulia-Gargano foreland in the Pleistocene, Geophys. Res. Lett., 19, 2275–2278, 1992.
Schettino, A. and Turco, E.: Tectonic history of the western Tethys since the Late Triassic, Geol. Soc. Am. Bull., 123, 89–105, 2011.
Schmid, S. M., Bernoulli, D., Fügenschuh, B., Maţenco, L., Schefer, S., Schuster, R., Tischler, M., and Ustaszewski, K.: The Alpine-Carpathian-Dinaridic orogenic system: correlation and evolution of tectonic units, Swiss J Geosci, 101, 139–183, 2008.
Schmid, S. M., Scharf, A., Handy, M. R., and Rosenberg, C. L.: The Tauern Window (Eastern Alps, Austria): a new tectonic map, with cross-sections and a tectonometamorphic synthesis, Swiss J. Geosci., 106, 1–32, 2013.
Schönborn, G.: Balancing cross sections with kinematic constraints: The Dolomites (northern Italy), Tectonics, 18, 527–545, 1999.
Scisciani, V. and Calamita, F.: Active intraplate deformation within Adria: Examples from the Adriatic region, Tectonophysics, 476, 57–72, 2009.
Scrocca, D.: Thrust front segmentation induced by differential slab retreat in the Apennines (Italy),, 18, 154–161, 2006.
Sengör, A. M. C., Yilmaz, Y., and Sungurlu, O.: Tectonics of the Mediterranean Cimmerides: nature and evolution of the western termination of Palaeo-Tethys, Geological Society, London, Special Publications, 17, 77–112, 1984.
Seton, M., Müller, R. D., Zahirovic, S., Gaina, C., Torsvik, T. H., Shephard, G., Talsma, A., Gurnis, M., Turner, M., Maus, S., and Chandler, M.: Global continental and ocean basin reconstructions since 200 Ma, Earth Sci. Rev., 113, 212–270, 2012.
Sinni, E. L. and Borgomano, J.: Le Crétacé supérieur des Murges sud-orientales (Italie méridionale): stratigraphie et évolution des paléoenvironnements, Rivista Italiana di Paleontologia e Stratigrafia, 95, 95–136, 1989.
Spalluto, L.: Facies evolution and sequence chronostratigraphy of a "mid-"Cretaceous shallow-water carbonate succession of the Apulia Carbonate Platform from the northern Murge area (Apulia, southern Italy), Facies, 58, 17–36, 2011.
Spalluto, L. and Caffau, M.: Stratigraphy of the mid-Cretaceous shallow-water limestones of the Apulia Carbonate Platform (Murge, Apulia, southern Italy), IJG, 129, 335–352, 2010.
Spalluto, L., Pieri, P., and Ricchetti, G.: Le facies carbonatiche di piattaforma interna del Promontorio del Gargano; implicazioni paleoambientali e correlazioni con la coeva successione delle Murge (Italia meridionale, Puglia), IJG, 124, 675–690, 2005.
Speranza, F. and Kissel, C.: First paleomagnetism of eocene rocks from Gargano: Widespread overprint or non rotation? Geophys. Res. Lett., 20, 2627–2630, 1993.
Speranza, F., Minelli, L., Pignatelli, A., and Chiappini, M.: The Ionian Sea: The oldest in situ ocean fragment of the world?, J. Geophys. Res., 117, B12101, https://doi.org/10.1029.2012JB009475, 2012.
Stampfli, G. M. and Borel, G. D.: A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons, Earth Planet. Sci. Lett., 196, 17–33, 2002.
Stampfli, G. M. and Hochard, C., Eds.: Plate tectonics of the Alpine realm, Geological Society, London, Special Publications, 327, 89–111, 2009.
Stampfli, G. M. and Mosar, J.: The making and becoming of Apulia, Mem. Sci. Geol., 51, 141–154, 1999.
Stojadinović, U., Matenco, L., and Andriessen, P.: The balance between orogenic building and subsequent extension during the Tertiary evolution of the NE Dinarides: Constraints from low-temperature thermochronology, Glob. Planet. Change, 103, 19–38, 2013.
Tauxe, L. and Kent, D. V.: A simplified statistical model for the geomagnetic field and the detection of shallow bias in paleomagnetic inclinations: Was the ancient magnetic field dipolar? Timescales of the Paleomagnetic field, Geophys. Monogr. Ser., 145, 101–115, 2004.
Torsvik, T. H., Van der Voo, R., Preeden, U., Mac Niocaill, C., Steinberger, B., Doubrovine, P. V., van Hinsbergen, D. J. J., Domeier, M., Gaina, C., Tohver, E., Meert, J. G., McCausland, P. J. A., and Cocks, L. R. M.: Phanerozoic polar wander, paleogeography and dynamics, Earth Sci. Rev., 114, 325–368, 2012.
Tozzi, M., Kissel, C., Funiciello, R., Laj, C., and Parotto, M.: A clockwise rotation of southern Apulia?, Geophys. Res. Lett., 15, 681–684, 1988.
Tropeano, M., Spalluto, L., Moretti, M., Pieri, P., and Sabato, L.: Depositi carbonatici infrapleistocenici di tipo Foramol in sestemi di scarpata (Salento-Italia Meridionale), Il Quaternario, 17, 537–546, 2004.
Underhill, J. R.: Late Cenozoic deformation of the Hellenide foreland, western Greece, Geol. Soc. Am. Bull., 101, 613–634, 1989.
Ustaszewski, K., Schmid, S. M., Fügenschuh, B., Tischler, M., Kissling, E. and Spakman, W.: A map-view restoration of the Alpine-Carpathian-Dinaridic system for the Early Miocene, Swiss J. Geosci., 101, 273–294, 2008.
Vai, G. B. and Martini, I. P.: Anatomy of an orogen: the Apennines and adjacent Mediterranean basins, Springer-science+business Media B.V., Dordrecht, 2001.
Vandenberg, J.: Reappraisal of paleomagnetic data from Gargano (South Italy), Tectonophysics, 98, 29–41, 1983.
van Hinsbergen, D. J. J. and Schmid, S. M.: Map view restoration of Aegean-West Anatolian accretion and extension since the Eocene, Tectonics, 31, TC5005, https://doi.org/10.1029/2012TC003132, 2012.
van Hinsbergen, D. J. J., van der Meer, D. G., Zachariasse, W. J., and Meulenkamp, J. E.: Deformation of western Greece during Neogene clockwise rotation and collision with Apulia, Internat. J. Earth Sci., 95, 463–490, 2006.
van Hinsbergen, D., Vissers, R., and Spakman, W.: Origin and consequences of western Mediterranean subduction, rollback, and slab segmentation, Tectonics, 33, 393–419, https://doi.org/10.1002/2013TC003349, 2014.
Vescogni, A.: Evoluzione delle biocostruzioni a vermetidi e loro utilizzo come "markers" paleobatimetrici e paleoclimatici, Giornale di Geologia, 62, 55–61, 2000.
Vissers, R., van Hinsbergen, D., and Meijer, P. T.: Kinematics of Jurassic ultra-slow spreading in the Piemonte Ligurian ocean, Earth Planet. Sci. Lett., 380, 138–150, 2013.
Vlahović, I., Tišljar, J., Velić, I., and Matičec, D.: Evolution of the Adriatic Carbonate Platform: Palaeogeography, main events and depositional dynamics, Palaeogeography, 220, 333–360, 2005.
Wortel, M. J. R. and Spakman, W.: Subduction and slab detachment in the Mediterranean-Carpathian region, Science, 290, 1910–1917, 2000.
Wortmann, U. G., Weissert, H., Funk, H., and Hauck, J.: Alpine plate kinematics revisited: The Adria Problem, Tectonics, 20, 134–147, 2001.
Zappaterra, E.: Carbonate paleogeographic sequences of the peradriatic region, Bolletino di Societa Geologica Italiana, 109, 5–20, 1990.
Zappaterra, E.: Source-Rock Distribution Model of the Periadriatic Region, AAPG Bulletin, 78, 333–354, 1994.
Zijderveld, J. D. A.: A.C. demagnetization of rocks: analysis of results, in Methods in Palaeomagnetism, Elsevier, Amsterdam, New York, 254–286, 1967.
