Articles | Volume 11, issue 4
https://doi.org/10.5194/se-11-1571-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/se-11-1571-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
On the morphology and amplitude of 2D and 3D thermal anomalies induced by buoyancy-driven flow within and around fault zones
Laurent Guillou-Frottier
CORRESPONDING AUTHOR
BRGM, Georesources Division, 45060, Orléans, France
ISTO, UMR7327, Université d'Orléans, CNRS, BRGM, 45071,
Orléans, France
Hugo Duwiquet
BRGM, Georesources Division, 45060, Orléans, France
ISTO, UMR7327, Université d'Orléans, CNRS, BRGM, 45071,
Orléans, France
TLS-Geothermics, 31200, Toulouse, France
Gaëtan Launay
Harquail School of Earth Sciences, Laurentian University, P3E2C6, Sudbury, Canada
Audrey Taillefer
CFG Services, 45060, Orléans, France
Vincent Roche
ISTEP, UMR7193, Sorbonne Université, CNRS-INSU, 75005, Paris,
France
Gaétan Link
GET, UMR 5563, Université Toulouse III-Paul Sabatier, CNRS, IRD,
CNES, 31400, Toulouse, France
Related authors
No articles found.
Laurent Jolivet, Laurent Arbaret, Laetitia Le Pourhiet, Florent Cheval-Garabédian, Vincent Roche, Aurélien Rabillard, and Loïc Labrousse
Solid Earth, 12, 1357–1388, https://doi.org/10.5194/se-12-1357-2021, https://doi.org/10.5194/se-12-1357-2021, 2021
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Although viscosity of the crust largely exceeds that of magmas, we show, based on the Aegean and Tyrrhenian Miocene syn-kinematic plutons, how the intrusion of granites in extensional contexts is controlled by crustal deformation, from magmatic stage to cold mylonites. We show that a simple numerical setup with partial melting in the lower crust in an extensional context leads to the formation of metamorphic core complexes and low-angle detachments reproducing the observed evolution of plutons.
Gaétan Milesi, Patrick Monié, Philippe Münch, Roger Soliva, Audrey Taillefer, Olivier Bruguier, Mathieu Bellanger, Michaël Bonno, and Céline Martin
Solid Earth, 11, 1747–1771, https://doi.org/10.5194/se-11-1747-2020, https://doi.org/10.5194/se-11-1747-2020, 2020
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This study proposes a new way to highlight hydrothermal fluid circulations and thermal anomalies in the Earth's crust with a combined evaluation of the age of granite and gneiss apatites (< 200 µm) as well as the behaviour of their chemical elements. As an exploration tool, this approach is very promising and complementary to other geothermal exploration techniques based on numerical modelling. Moreover, it is a cost-effective tool as it allows for constraining geothermal models.
Related subject area
Subject area: The evolving Earth surface | Editorial team: Seismics, seismology, paleoseismology, geoelectrics, and electromagnetics | Discipline: Geophysics
Seismic wave modeling of fluid-saturated fractured porous rock: including fluid pressure diffusion effects of discretely distributed large-scale fractures
Integration of automatic implicit geological modelling in deterministic geophysical inversion
Ground motion emissions due to wind turbines: observations, acoustic coupling, and attenuation relationships
Seismic amplitude response to internal heterogeneity of mass-transport deposits
Investigation of the effects of surrounding media on the distributed acoustic sensing of a helically wound fibre-optic cable with application to the New Afton deposit, British Columbia
Geophysical analysis of an area affected by subsurface dissolution – case study of an inland salt marsh in northern Thuringia, Germany
An efficient probabilistic workflow for estimating induced earthquake parameters in 3D heterogeneous media
Dynamic motion monitoring of a 3.6 km long steel rod in a borehole during cold-water injection with distributed fiber-optic sensing
On the comparison of strain measurements from fibre optics with a dense seismometer array at Etna volcano (Italy)
The impact of seismic interpretation methods on the analysis of faults: a case study from the Snøhvit field, Barents Sea
Integrated land and water-borne geophysical surveys shed light on the sudden drying of large karst lakes in southern Mexico
Characterizing a decametre-scale granitic reservoir using ground-penetrating radar and seismic methods
Upper Jurassic carbonate buildups in the Miechów Trough, southern Poland – insights from seismic data interpretations
New regional stratigraphic insights from a 3D geological model of the Nasia sub-basin, Ghana, developed for hydrogeological purposes and based on reprocessed B-field data originally collected for mineral exploration
Characterisation of subglacial water using a constrained transdimensional Bayesian transient electromagnetic inversion
Subsurface characterization of a quick-clay vulnerable area using near-surface geophysics and hydrological modelling
Electrical formation factor of clean sand from laboratory measurements and digital rock physics
Drill bit noise imaging without pilot trace, a near-surface interferometry example
Calibrating a new attenuation curve for the Dead Sea region using surface wave dispersion surveys in sites damaged by the 1927 Jericho earthquake
Shear wave reflection seismic yields subsurface dissolution and subrosion patterns: application to the Ghor Al-Haditha sinkhole site, Dead Sea, Jordan
Yingkai Qi, Xuehua Chen, Qingwei Zhao, Xin Luo, and Chunqiang Feng
Solid Earth, 15, 535–554, https://doi.org/10.5194/se-15-535-2024, https://doi.org/10.5194/se-15-535-2024, 2024
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Fractures tend to dominate the mechanical and hydraulic properties of porous rock and impact the scattering characteristics of passing waves. This study takes into account the poroelastic effects of fractures in numerical modeling. Our results demonstrate that scattered waves from complex fracture systems are strongly affected by the fractures.
Jérémie Giraud, Guillaume Caumon, Lachlan Grose, Vitaliy Ogarko, and Paul Cupillard
Solid Earth, 15, 63–89, https://doi.org/10.5194/se-15-63-2024, https://doi.org/10.5194/se-15-63-2024, 2024
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We present and test an algorithm that integrates geological modelling into deterministic geophysical inversion. This is motivated by the need to model the Earth using all available data and to reconcile the different types of measurements. We introduce the methodology and test our algorithm using two idealised scenarios. Results suggest that the method we propose is effectively capable of improving the models recovered by geophysical inversion and may be applied in real-world scenarios.
Laura Gaßner and Joachim Ritter
Solid Earth, 14, 785–803, https://doi.org/10.5194/se-14-785-2023, https://doi.org/10.5194/se-14-785-2023, 2023
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In this work we analyze signals emitted from wind turbines. They induce sound as well as ground motion waves which propagate through the subsurface and are registered by sensitive instruments. In our data we observe when these signals are present and how strong they are. Some signals are present in ground motion and sound data, providing the opportunity to study similarities and better characterize emissions. Furthermore, we study the amplitudes with distance to improve the signal prediction.
Jonathan Ford, Angelo Camerlenghi, Francesca Zolezzi, and Marilena Calarco
Solid Earth, 14, 137–151, https://doi.org/10.5194/se-14-137-2023, https://doi.org/10.5194/se-14-137-2023, 2023
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Submarine landslides commonly appear as low-amplitude zones in seismic data. Previous studies have attributed this to a lack of preserved internal structure. We use seismic modelling to show that an amplitude reduction can be generated even when there is still metre-scale internal structure, by simply deforming the bedding. This has implications for interpreting failure type, for core-seismic correlation and for discriminating landslides from other "transparent" phenomena such as free gas.
Sepidehalsadat Hendi, Mostafa Gorjian, Gilles Bellefleur, Christopher D. Hawkes, and Don White
Solid Earth, 14, 89–99, https://doi.org/10.5194/se-14-89-2023, https://doi.org/10.5194/se-14-89-2023, 2023
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In this study, the modelling results are used to help understand the performance of a helically wound fibre (HWC) from a field study at the New Afton mine, British Columbia. We introduce the numerical 3D model to model strain values in HWC to design more effective HWC system. The DAS dataset at New Afton, interpreted in the context of our modelling, serves as a practical demonstration of the extreme effects of surrounding media and coupling on HWC data quality.
Sonja H. Wadas, Hermann Buness, Raphael Rochlitz, Peter Skiba, Thomas Günther, Michael Grinat, David C. Tanner, Ulrich Polom, Gerald Gabriel, and Charlotte M. Krawczyk
Solid Earth, 13, 1673–1696, https://doi.org/10.5194/se-13-1673-2022, https://doi.org/10.5194/se-13-1673-2022, 2022
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The dissolution of rocks poses a severe hazard because it can cause subsidence and sinkhole formation. Based on results from our study area in Thuringia, Germany, using P- and SH-wave reflection seismics, electrical resistivity and electromagnetic methods, and gravimetry, we develop a geophysical investigation workflow. This workflow enables identifying the initial triggers of subsurface dissolution and its control factors, such as structural constraints, fluid pathways, and mass movement.
La Ode Marzujriban Masfara, Thomas Cullison, and Cornelis Weemstra
Solid Earth, 13, 1309–1325, https://doi.org/10.5194/se-13-1309-2022, https://doi.org/10.5194/se-13-1309-2022, 2022
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Induced earthquakes are natural phenomena in which the events are associated with human activities. Although the magnitudes of these events are mostly smaller than tectonic events, in some cases, the magnitudes can be high enough to damage buildings near the event's location. To study these (high-magnitude) induced events, we developed a workflow in which the recorded data from an earthquake are used to describe the source and monitor the area for other (potentially high-magnitude) earthquakes.
Martin Peter Lipus, Felix Schölderle, Thomas Reinsch, Christopher Wollin, Charlotte Krawczyk, Daniela Pfrang, and Kai Zosseder
Solid Earth, 13, 161–176, https://doi.org/10.5194/se-13-161-2022, https://doi.org/10.5194/se-13-161-2022, 2022
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A fiber-optic cable was installed along a freely suspended rod in a deep geothermal well in Munich, Germany. A cold-water injection test was monitored with fiber-optic distributed acoustic and temperature sensing. During injection, we observe vibrational events in the lower part of the well. On the basis of a mechanical model, we conclude that the vibrational events are caused by thermal contraction of the rod. The results illustrate potential artifacts when analyzing downhole acoustic data.
Gilda Currenti, Philippe Jousset, Rosalba Napoli, Charlotte Krawczyk, and Michael Weber
Solid Earth, 12, 993–1003, https://doi.org/10.5194/se-12-993-2021, https://doi.org/10.5194/se-12-993-2021, 2021
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We investigate the capability of distributed acoustic sensing (DAS) to record dynamic strain changes related to Etna volcano activity in 2019. To validate the DAS measurements, we compute strain estimates from seismic signals recorded by a dense broadband array. A general good agreement is found between array-derived strain and DAS measurements along the fibre optic cable. Localised short wavelength discrepancies highlight small-scale structural heterogeneities in the investigated area.
Jennifer E. Cunningham, Nestor Cardozo, Chris Townsend, and Richard H. T. Callow
Solid Earth, 12, 741–764, https://doi.org/10.5194/se-12-741-2021, https://doi.org/10.5194/se-12-741-2021, 2021
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This work investigates the impact of commonly used seismic interpretation methods on the analysis of faults. Fault analysis refers to fault length, displacement, and the impact these factors have on geological modelling and hydrocarbon volume calculation workflows. This research was conducted to give geoscientists a better understanding of the importance of interpretation methods and the impact of unsuitable methology on geological analyses.
Matthias Bücker, Adrián Flores Orozco, Jakob Gallistl, Matthias Steiner, Lukas Aigner, Johannes Hoppenbrock, Ruth Glebe, Wendy Morales Barrera, Carlos Pita de la Paz, César Emilio García García, José Alberto Razo Pérez, Johannes Buckel, Andreas Hördt, Antje Schwalb, and Liseth Pérez
Solid Earth, 12, 439–461, https://doi.org/10.5194/se-12-439-2021, https://doi.org/10.5194/se-12-439-2021, 2021
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We use seismic, electromagnetic, and geoelectrical methods to assess sediment thickness and lake-bottom geology of two karst lakes. An unexpected drainage event provided us with the unusual opportunity to compare water-borne measurements with measurements carried out on the dry lake floor. The resulting data set does not only provide insight into the specific lake-bottom geology of the studied lakes but also evidences the potential and limitations of the employed field methods.
Joseph Doetsch, Hannes Krietsch, Cedric Schmelzbach, Mohammadreza Jalali, Valentin Gischig, Linus Villiger, Florian Amann, and Hansruedi Maurer
Solid Earth, 11, 1441–1455, https://doi.org/10.5194/se-11-1441-2020, https://doi.org/10.5194/se-11-1441-2020, 2020
Łukasz Słonka and Piotr Krzywiec
Solid Earth, 11, 1097–1119, https://doi.org/10.5194/se-11-1097-2020, https://doi.org/10.5194/se-11-1097-2020, 2020
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This paper shows the results of seismic interpretations that document the presence of large Upper Jurassic carbonate buildups in the Miechów Trough (S Poland). Our work fills the gap in recognition of the Upper Jurassic carbonate depositional system of southern Poland. The results also provide an excellent generic reference point, showing how and to what extent seismic data can be used for studies of carbonate depositional systems, in particular for the identification of the carbonate buildups.
Elikplim Abla Dzikunoo, Giulio Vignoli, Flemming Jørgensen, Sandow Mark Yidana, and Bruce Banoeng-Yakubo
Solid Earth, 11, 349–361, https://doi.org/10.5194/se-11-349-2020, https://doi.org/10.5194/se-11-349-2020, 2020
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Time-domain electromagnetic (TEM) geophysics data originally collected for mining purposes were reprocessed and inverted. The new inversions were used to construct a 3D model of the subsurface geology to facilitate hydrogeological investigations within a DANIDA-funded project. Improved resolutions from the TEM enabled the identification of possible paleovalleys of glacial origin, suggesting the need for a reevaluation of the current lithostratigraphy of the Voltaian sedimentary basin.
Siobhan F. Killingbeck, Adam D. Booth, Philip W. Livermore, C. Richard Bates, and Landis J. West
Solid Earth, 11, 75–94, https://doi.org/10.5194/se-11-75-2020, https://doi.org/10.5194/se-11-75-2020, 2020
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This paper presents MuLTI-TEM, a Bayesian inversion tool for inverting TEM data with independent depth constraints to provide statistical properties and uncertainty analysis of the resistivity profile with depth. MuLTI-TEM is highly versatile, being compatible with most TEM survey designs, ground-based or airborne, along with the depth constraints being provided from any external source. Here, we present an application of MuLTI-TEM to characterise the subglacial water under a Norwegian glacier.
Silvia Salas-Romero, Alireza Malehmir, Ian Snowball, and Benoît Dessirier
Solid Earth, 10, 1685–1705, https://doi.org/10.5194/se-10-1685-2019, https://doi.org/10.5194/se-10-1685-2019, 2019
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Land–river reflection seismic, hydrogeological modelling, and magnetic investigations in an area prone to quick-clay landslides in SW Sweden provide a detailed description of the subsurface structures, such as undulating fractured bedrock, a sedimentary sequence of intercalating leached and unleached clay, and coarse-grained deposits. Hydrological properties of the coarse-grained layer help us understand its role in the leaching process that leads to the formation of quick clays in the area.
Mohammed Ali Garba, Stephanie Vialle, Mahyar Madadi, Boris Gurevich, and Maxim Lebedev
Solid Earth, 10, 1505–1517, https://doi.org/10.5194/se-10-1505-2019, https://doi.org/10.5194/se-10-1505-2019, 2019
Mehdi Asgharzadeh, Ashley Grant, Andrej Bona, and Milovan Urosevic
Solid Earth, 10, 1015–1023, https://doi.org/10.5194/se-10-1015-2019, https://doi.org/10.5194/se-10-1015-2019, 2019
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Data acquisition costs mainly borne by expensive vibrator machines (i.e., deployment, operations, and maintenance) can be regarded as the main impediment to wide application of seismic methods in the mining industry. Here, we show that drill bit noise can be used to image the shallow subsurface when it is optimally acquired and processed. Drill bit imaging methods have many applications in small scale near-surface projects, such as those in mining exploration and geotechnical investigation.
Yaniv Darvasi and Amotz Agnon
Solid Earth, 10, 379–390, https://doi.org/10.5194/se-10-379-2019, https://doi.org/10.5194/se-10-379-2019, 2019
Ulrich Polom, Hussam Alrshdan, Djamil Al-Halbouni, Eoghan P. Holohan, Torsten Dahm, Ali Sawarieh, Mohamad Y. Atallah, and Charlotte M. Krawczyk
Solid Earth, 9, 1079–1098, https://doi.org/10.5194/se-9-1079-2018, https://doi.org/10.5194/se-9-1079-2018, 2018
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The alluvial fan of Ghor Al-Haditha (Dead Sea) is affected by subsidence and sinkholes. Different models and hypothetical processes have been suggested in the past; high-resolution shear wave reflection surveys carried out in 2013 and 2014 showed the absence of evidence for a massive shallow salt layer as formerly suggested. Thus, a new process interpretation is proposed based on both the dissolution and physical erosion of Dead Sea mud layers.
Cited articles
Achtziger-Putančič, P., Loew, S., Hiller, A., and Mariethoz, G.: 3D
fluid flow in fault zones of crystalline basement rocks
(Poehla-Tellerhaeuser Ore Field, Ore Mountains, Germany), Geofluids, 16,
688–710, https://doi.org/10.1111/gfl.12192, 2016.
Achtziger-Putančič, P., Loew, S., and Hiller, A.: Factors
controlling the permeability distribution in fault vein zones surrounding
granitic intrusions (Ore Mountains/Germany), J. Geophys. Res., 122,
1876–1899, https://doi.org/10.1002/2016JB013619, 2017.
Ague, J. J.: Fluid flow in the deep crust, Treatise on geochemistry, 2nd
Edn., Elsevier, 203–247, https://doi.org/10.1016/B9780-08-095975-7.00306-5,
2014.
Andersen, C., Rüpke, L., Hasenclever, J., Grevemeyer, I., and Petersen,
S.: Fault geometry and permeability contrast control vent temperatures at
the Logatchev 1 hydrothermal field, Mid-Atlantic Ridge, Geology, 43, 51–54,
https://doi.org/10.1130/G36113.1, 2015.
Artemieva, I. M., Thybo, H., Jakobsen, K., Sorensen, N. K., and Nielsen, L. S. K.:
Heat production in granitic rocks: Global analysis based on a new data
compilation GRANITE2017, Earth Sci. Rev., 172, 1–26, https://doi.org/10.1016/j.earscirev.2017.07.003, 2017.
Bächler, D., Kohl, T., and Rybach, L.: Impact of graben-parallel faults
on hydrothermal convection – RhineGraben case study, Phys. Chem. Earth, 28,
431–441, https://doi.org/10.1016/S1474-7065(03)00063-9, 2003.
Baietto, A., Cadoppi, P., Martinotti, G., Perello, P., Perrochet, P., and
Vuataz, F.-D.: Assessment of thermal circulations in strike–slip fault
systems: the Terme di Valdieri case (Italian western Alps), Geol. Soc.
Spec. Pub., 299, 317–339, https://doi.org/10.1144/SP299.19,
2008.
Bartels, A., Behrens, H., Holtz, F., Schmidt, B.C., Fechtelkord, M.,
Knipping, J., Crede, L., Baasner, A., and Pukallus, N.: The effect of
fluorine, boron and phosphorus on the viscosity of pegmatite forming melts,
Chem. Geol., 346, 184–198, https://doi.org/10.1016/j.chemgeo.2012.09.024, 2013.
Bauer, J. F., Krumbholz, M., Luijendijk, E., and Tanner, D. C.: A numerical sensitivity study of how permeability, porosity, geological structure, and hydraulic gradient control the lifetime of a geothermal reservoir, Solid Earth, 10, 2115–2135, https://doi.org/10.5194/se-10-2115-2019, 2019.
Bense, V. F., Gleeson, T., Loveless, S. E., Bour, O., and Scibek, J.: Fault
zone hydrogeology, Earth Sci. Rev., 127, 171–192, https://doi.org/10.1016/j.earscirev.2013.09.008, 2013.
Blackwell, D. D., Netragu, P. T., and Richards, M.: Assessment of the Enhanced
Geothermal System resource base of the United States, Nat. Resour. Res.,
15, 283–308, https://doi.org/10.1007/s11053-007-9028-7, 2006.
Boiron, M.-C., Cathelineau, M., Banks, D. A., Fourcade, S., and Vallance,
J.: Mixing of metamorphic and surficial fluids during the uplift of the
Hercynian upper crust: consequences for gold deposition, Chem. Geol., 194,
119–141, https://doi.org/10.1016/S0009-2541(02)00274-7, 2003.
Bonnemaison, M. and Marcoux, E.: Auriferous mineralization in some
shear-zones: A three-stage model of metallogenesis, Mineral. Deposita, 25,
96–104, https://doi.org/10.1007/BF00208851, 1990.
Bonté, D., Guillou-Frottier, L., Garibaldi, C., Bourgine, B., Lopez, S.,
Bouchot, V., and Lucazeau, F.: Subsurface temperature maps in French
sedimentary basins: new data compilation and interpolation, B. Soc. Geol.
Fr., 181, 377–390, https://doi.org/10.2113/gssgfbull.181.4.377,
2010.
Clauser, C. and Villinger, H.: Analysis of conductive and convective heat
transfer in a sedimentary basin, demonstrated for the Rheingraben, Geophys.
J. Int., 100, 393–414, https://doi.org/10.1111/j.1365-246X.1990.tb00693.x, 1990.
Cloetingh, S., van Wees, J.D., Ziegler, P.A., Lenkey, L., Beekman, F.,
Tesauro, M., Förster, A., Norden, B., Kaban, M., Hardebol, N.,
Bonté, D., Genter, A., Guillou-Frottier, L., TerVoorde, M., Sokoutis,
D., Willingshofer, E., Cornu, T., and Worum, G.: Lithosphere tectonics and
thermo-mechanical properties: An integrated modelling approach for Enhanced
Geothermal Systems exploration in Europe, Earth Sci. Rev., 102, 159–206,
https://doi.org/10.1016/j.earscirev.2010.05.003, 2010.
Coelho, G., Branquet, Y., Sizaret, S., Arbaret, L., Champallier, R., and
Rozenbaum, O.: Permeability of sheeted dykes beneath oceanic ridges: Strain
experiments coupled with 3D numericalmodeling of the Troodos Ophiolite,
Cyprus, Tectonophysics, 644–645, 138–150, https://doi.org/10.1016/j.tecto.2015.01.004, 2015.
Coumou, D., Driesner, T., Geiger, S., Heinrich, C. A., and Matthäi, S.:
The dynamics of mid-ocean ridge hydrothermal systems: splitting plumes and
fluctuating vent temperatures, Earth Planet. Sc. Lett., 245, 218–231,
https://doi.org/10.1016/j.epsl.2006.02.044, 2006.
Coumou, D., Driesner, T., Geiger, S., Paluszny, A., and Heinrich, C. A.:
High-resolution three-dimensional simulations of mid-ocean ridge
hydrothermal systems, J. Geophys. Res., 114, B07104, https://doi.org/10.1029/2008JB006121, 2009.
Cox, S. F.: The application of failure mode diagrams for exploring the roles
of fluid pressure and stress states in controlling styles of
fracture-controlled permeability enhancement in faults and shear zones,
Geofluids, 10, 217–233, https://doi.org/10.1111/j.1468-8123.2010.00281.x, 2010.
Curewitz, D. and Karson, J. A.: Structural settings of hydrothermal outflow:
Fracture permeability maintained by fault propagation and interaction, J.
Volcanol. Geoth. Res., 79, 149–168, https://doi.org/10.1016/S0377-0273(97)00027-9, 1997.
Della Vedova, B., Vecellio, C., Bellani, S., and Tinivella, U.: Thermal
modelling of the Larderello geothermal field (Tuscany, Italy), Int. J. Earth
Sci., 97, 317–332, https://doi.org/10.1007/s00531-007-0249-0,
2008.
Deveaud, S., Guillou-Frottier, L., Millot, R., Gloaguen, E., Branquet, Y.,
Villaros, A., Pichavant, M., and Barbosa da Silva, D.: Innovative and
multi-disciplinary approach for discussing the emplacement of Variscan
LCT-pegmatite fields, Proceedings of the 13th SGA Biennal Meeting, Nancy,
France, 24–27 August 2015, Vol. 2, Asga-Assoc scientifique geologie and applications, Nancy, France, 717–720, 2015.
Duwiquet, H., Arbaret, L., Guillou-Frottier, L., Heap, M. J., and Bellanger,
M.: On the geothermal potential of crustal fault zones: a case study from
the Pontgibaud area (French Massif Central, France), Geotherm. Energy, 2019,
7–33, https://doi.org/10.1186/s40517-019-0150-7, 2019.
Erkan, K.: Geothermal investigations in western Anatolia using equilibrium temperatures from shallow boreholes, Solid Earth, 6, 103–113, https://doi.org/10.5194/se-6-103-2015, 2015.
Faulds, J., Coolbaugh, M., Bouchot, V., Moeck, I., and Oğuz, K.:
Characterizing structural controls of geothermal reservoirs in the Great
Basin, USA, and western Turkey: developing successful exploration strategies
in extended terranes, Proceedings World Geothermal Congress, Bali,
Indonesia, 25–29 April 2010, 11 pp., 2010.
Faulkner, D. R., Jackson, C. A. L., Lunn, R. J., Schlische, R. W., Shipton, Z. K.,
Wibberley, C. A. J., and Withjack, M. O.: A review of recent developments
concerning the structure, mechanics and fluid flow properties of fault
zones, J. Struct. Geol., 32, 1557–1575, https://doi.org/10.1016/j.jsg.2010.06.009, 2010.
Fehn, U., Cathles, L., and Holland, H. D.: Hydrothermal convection and
uranium deposits in abnormally radioactive plutons, Econ. Geol., 73,
1556–1566, https://doi.org/10.2113/gsecongeo.73.8.1556, 1978.
Fontaine, F. J. and Wilcock, W. S. D.: Two-dimensional numerical models of
open-top hydrothermal convection at high Rayleigh and Nusselt numbers:
Implications for mid-ocean ridge hydrothermal circulation, Geochem. Geophy.
Geosy., 8, Q07010, https://doi.org/10.1029/2007GC001601, 2007.
Fontaine, F. J., Rabinowicz, M., and Boulègue, J.: Permeability changes
due to mineral diagenesis in fractured crust: implications for hydrothermal
circulation at mid-ocean ridges, Earth Planet. Sc. Lett., 184, 407–425,
https://doi.org/10.1016/S0012-821X(00)00332-0, 2001.
Forster, C. and Smith, L.: The influence of groundwater flow on thermal
regimes in mountainous terrain: a model study, J. Geophys. Res., 94,
9439–9451, https://doi.org/10.1029/JB094iB07p09439, 1989.
Garibaldi, C., Guillou-Frottier, L., Lardeaux, J.-M., Bonté, D., Lopez,
S., Bouchot, V., and Ledru, P.: Thermal anomalies and geological structures
in the Provence basin: implications for hydrothermal circulations at depth,
B. Soc. Geol. Fr., 181, 363–376, https://doi.org/10.2113/gssgfbull.181.4.363, 2010.
Gerdes, M., Baumgartner, L. P., and Person, M.: Convective fluid flow
through heterogeneous country rocks during contact metamorphism, J. Geophys.
Res., 103, 23983–24003, https://doi.org/10.1029/98JB02049, 1998.
Gourcerol, B., Kontak, D. J., Petrus, J. A., and Thurston, P. C.: Application of
LA ICP-MS analysis of arsenopyrite to gold metallogeny of the Meguma
Terrane, Nova Scotia, Canada, Gondwana Res., 81, 265–290, https://doi.org/10.1016/j.gr.2019.11.011, 2020.
Guillou-Frottier, L., Carré, C., Bourgine, B., Bouchot, V., and Genter,
A.: Structure of hydrothermal convection in the Upper Rhine Graben as
inferred from corrected temperature data and basin-scale numerical models,
J. Volcanol. Geoth. Res., 256, 29–49, https://doi.org/10.1016/j.jvolgeores.2013.02.008, 2013.
Harcouët-Menou, V., Guillou-Frottier, L., Bonneville, A., Adler, P. M.,
and Mourzenko, V.: Hydrothermal convection in and around mineralized fault
zones: insights from two- and three-dimensional numerical modeling applied
to the Ashanti belt, Ghana, Geofluids, 9, 116–137, https://doi.org/10.1111/j.1468-8123.2009.00247.x, 2009.
Howald, T., Person, M., Campbell, A., Lueth, V., Hofstra, A., Sweetkind, D.,
Gable, C. W., Banerjee, A., Luijendijk, E., Crossey, L., Karlstrom, K.,
Kelley, S., and Philipps, F. M.: Evidence for long timescale (>103 years) changes in hydrothermal activity induced by seismic events,
Geofluids, 15, 252–268, https://doi.org/10.1111/gfl.12113, 2015.
Hutnak, M., Hurwitz, S., Ingebritsen, S. E., and Hsieh, P. A.: Numerical
models of caldera deformation: Effects of multiphase and multicomponent
hydrothermal fluid flow, J. Geophys. Res., 114, B04411, https://doi.org/10.1029/2008JB006151, 2009.
Ingebritsen, S. E. and Appold, M. S.: The physical hydrogeology of ore
deposits, Econ. Geol., 107, 559–584, https://doi.org/10.2113/econgeo.107.4.559, 2012.
Ingebritsen, S. E. and Gleeson, T.: Crustal permeability: introduction to
the special issue, Geofluids, 15, 1–10, https://doi.org/10.1111/gfl.12118, 2015.
Jammes, S., Huismans, R. S., and Muñoz, J. A.: Lateral variation in
structural style of mountain building: controls of rheological and rift
inheritance, Terra Nova, 26, 201–207, https://doi.org/10.1111/ter.12087, 2013.
Jamtveit, B., Putnis, C. V., and Malthe-Sorenssen, A.: Reaction induced
fracturing during replacement processes, Contrib. Mineral. Petrol., 157,
127–133, https://doi.org/10.1007/s00410-008-0324-y, 2009.
Jaupart, C. and Mareschal, J.-C.: Heat generation and transport in the
Earth, Cambridge University Press, New York, 464 pp., 2011.
Jupp, T. and Schultz, A.: A thermodynamic explanation for black smoker
temperatures, Nature, 403, 880–883, https://doi.org/10.1038/35002552, 2000.
Kuhn, M., Dobert, F., and Gessner, K.: Numerical investigation of the effect
of heterogeneous permeability distributions on free convection in the
hydrothermal system at Mount Isa, Australia, Earth Planet. Sc. Lett., 244,
655–671, https://doi.org/10.1016/j.epsl.2006.02.041, 2006.
Lapwood, E. R.: Convection of a fluid in a porous medium, Math. Proc.
Cambridge, 44, 508–521, https://doi.org/10.1017/S030500410002452X, 1948.
Launay, G.: Hydrodynamique des systèmes minéralisés
péri-granitiques: étude du gisement à W-Sn-(Cu) de Panasqueira
(Portugal), PhD thesis, University of Orléans, France, 514 pp., available at:
https://tel.archives-ouvertes.fr/tel-02101051 (last access: 24 August 2020), 2018.
Launay, G., Sizaret, S., Guillou-Frottier, L., Fauguerolles, C.,
Champallier, R., and Gloaguen, E.: Dynamic permeability related to
greisenization reactions in Sn-W ore deposits: quantitative petrophysical
and experimental evidence, Geofluids, 2019, 5976545, 2
https://doi.org/10.1155/2019/5976545, 2019.
Lawley, C. J. M., Creaser, R. A., Jackson, S. E., Yang, Z., Davis, B. J.,
Pehrsson, S. J., Dubé, B., Mercier-Langevin, P., and Vaillancourt, D.:
Unraveling the western Churchill Province Paleoproterozoic gold metallotect:
constraints from Re-Os arsenopyrite and U-Pb xenotime geochronology and
LA-ICP-MS arsenopyrite trace element chemistry at the BIF-hosted Meliadine
gold district, Nunavut, Canada, Econ. Geol., 110, 1425–1454, https://doi.org/10.2113/econgeo.110.6.1425, 2015.
Lin, G., Zhao, C., Hobbs, B. E., Ord, A., and Mühlhaus, H. B.:
Theoretical and numerical analyses of convective instability in porous media
with temperature-dependent viscosity, Commun. Numer. Meth. En., 19,
787–799, https://doi.org/10.1002/cnm.620, 2003.
Link, G., Vanderhaeghe, O., Béziat, D., de Saint Blanquat, M., Munoz,
M., Estrade, G., Guillou-Frottier, L., Gloaguen, E., Lahfid, A., and Melleton,
J.: Thermal peak detected in gold-bearing shear zones by a thermo-structural
study: a new tool to retrieve fluid flow?, Proceedings of the 15th SGA
Biennal Meeting, Glasgow, Scotland, 27–30 August 2019, Vol. 1, 260–263, Soc. Geology Applied Mineral Deposits-SGA,
2019.
Linstrom, P. J. and Mallard, W. G.: The NIST Chemistry WebBook: a chemical
data resource on the internet, J. Chem. Eng. Data, 46, 1059–1063, https://doi.org/10.1021/je000236i, 2001.
López, D. L. and Smith, L.: Fluid flow in fault zones: Analysis of the
interplay of convective circulation and topographically driven groundwater
flow, Water Resour. Res., 31, 1489–1503, https://doi.org/10.1029/95WR00422, 1995.
Lopez, T., Antoine, R., Kerr, Y., Darrozes, J., Rabinowicz, M., Ramillien,
G., Cazenave, A., and Genthon, P.: Subsurface Hydrology of the Lake Chad
Basin from Convection Modelling and Observations, Surv. Geophys., 37,
471–502, https://doi.org/10.1007/s10712-016-9363-5, 2016.
Louis, S., Luijendijk, E., Dunkl, I., and Person, M.: Episodic fluid flow in an
active fault, Geology, 47, 938–942, https://doi.org/10.1130/G46254.1, 2019.
Lowell, R. P., Van Cappellen, P., and Germanovich, L. N.: Silica Precipitation
in Fractures and the Evolution of Permeability in Hydrothermal Upflow Zone,
Science, 260, 192–194, https://doi.org/10.1126/science.260.5105.192, 1993.
Magri, F., Inbar, N., Siebert, C., Rosenthal, E., Guttman, J., and
Möller, P.: Transient simulations of large-scale hydrogeological
processes causing temperature and salinity anomalies in the Tiberias Basin,
J. Hydrol., 520, 342–355, https://doi.org/10.1016/j.jhydrol.2014.11.055, 2015.
Magri, F., Möller, S., Inbar, N., Möller, P., Raggad, M.,
Rödiger, T., Rosenthal, E., and Siebert, C.: 2D and 3D coexisting modes
of thermal convection in fractured hydrothermal systems – Implications for
transboundary flow in the Lower Yarmouk Gorge, Mar. Petrol. Geol., 78,
750–758, https://doi.org/10.1016/j.marpetgeo.2016.10.002, 2016.
Magri, F., Cacace, M., Fischer, T., Kolditz, O., Wanf, W., and Watanabe, N.:
Thermal convection of viscous fluids in a faulted system: 3D benchmark for
numerical codes, Enrgy. Proced., 125, 310–317, https://doi.org/10.1016/j.egypro.2017.08.204, 2017.
Malkovski, V. I. and Magri, F.: Thermal convection of temperature-dependent
viscous fluids within three-dimensional faulted geothermal systems:
estimation from linear and numerical analyses, Water Resour. Res., 52, 1–13,
https://doi.org/10.1002/2015WR018001, 2016.
Manning, C. E. and Ingebristen, S. E.: Permeability of the continental crust:
implications of geothermal data and metamorphic systems, Rev. Geophys., 37,
127–150, https://doi.org/10.1029/1998RG900002, 1999.
McKenna, J. R. and Blackwell, D. D.: Numerical modeling of transient Basin
and Range extensional geothermal systems, Geothermics, 33, 457–476,
https://doi.org/10.1016/j.geothermics.2003.10.001, 2000.
McLellan, J. G., Oliver, N. H. S., Hobbs, B. E., and Rowland, J. V.:
Modelling fluid convection stability in continental faulted rifts with
applications to the Taupo Volcanic Zone, New Zealand, J. Volcanol. Geoth.
Res., 190, 109–122, https://doi.org/10.1016/j.jvolgeores.2009.11.015, 2010.
Melleton, J., Gloaguen, E., and Frei, D.: Rare-elements (Li-Be-Ta-Sn-Nb)
magmatism in the European Variscan belt, a review, Proceedings of the 13th
SGA Biennal Meeting, Nancy, France, 24–27 August 2015, Vol. 2, Asga-Assoc scientifique geologie and applications, Nancy, France, 807–810,
2015.
Mezon, C., Mourzenko, V. V., Thovert, J.-F., Antoine, R., Fontaine, F.,
Finizola, A., and Adler, P. M.: Thermal convection in three-dimensional
fractured porous media, Phys. Rev., E97, 013106, https://doi.org/10.1103/PhysRevE.97.013106, 2018.
Mezri, L., Le Pourhiet, L., and Burov, E.: New parametric implementation of
metamorphic reactions limited by water content, impact on exhumation along
detachment faults, Lithos, 236–237, 287–298, https://doi.org/10.1016/j.lithos.2015.08.021, 2015.
Micklethwaite, S., Ford, A., Witt, W., and Sheldon, H. A.: The where and how
of faults, fluids and permeability – insights from fault stepovers, scaling
properties and gold mineralisation, Geofluids, 15, 240–251, https://doi.org/10.1111/gfl.12102, 2015.
Moeck, I. S.: Catalog of geothermal play types based on geologic controls,
Renew. Sust. Energ. Rev., 37, 867–882, https://doi.org/10.1016/j.rser.2014.05.032, 2014.
Patterson, J. W., Driesner, T., Matthai, S., and Tomlinson, R.: Heat and
fluid transport induced by convective fluid circulation within a fracture or
fault, J. Geophys. Res., 123, 2658–2673, https://doi.org/10.1002/2017JB015363, 2018a.
Patterson, J. W., Driesner, T., and Matthai, S. K.: Self-organizing fluid
convection patterns in an en echelon fault array, Geophys. Res. Lett., 45,
4799–4808, https://doi.org/10.1029/2018GL078271, 2018b.
Pepin, J., Person, M., Phillips, F., Kelley, S., Timmons, S., Owens, L.,
Witcher, J., and Gable, C.: Deep fluid circulation within crystalline
basement rocks and the role of hydrologic windows in the formation of the
Truth or Consequences, New Mexico low-temperature geothermal system,
Geofluids, 15, 139–160, https://doi.org/10.1111/gfl.12111, 2015.
Person, M., Hofstra, A., Sweetkind, D., Stone, W., Cohen, D., Gable, C. W.,
and Banerjee, A.: Analytical and numerical models of hydrothermal fluid flow
at fault intersections, Geofluids, 12, 312–326, https://doi.org/10.1111/gfl.12002, 2012.
Rabinowicz, M., Boulègue, J., and Genthon, P.: Two- and
three-dimentional modeling of hydrothermal convection in the sedimented
Middle Valley segment, Juan de Fuca Ridge, J. Geophys. Res., 103,
24045–24065, https://doi.org/10.1029/98JB01484, 1998.
Roche, V., Sternai, P., Guillou-Frottier, L., Menant, A., Jolivet, L.,
Bouchot, V., and Gerya, T.: Emplacement of metamorphic core complexes and
associated geothermal systems controlled by slab dynamics, Earth Planet.
Sc. Lett., 498, 322–333, https://doi.org/10.1016/j.epsl.2018.06.043, 2018.
Roche, V., Bouchot, V., Beccaletto, L., Jolivet, L., Guillou-Frottier, L.,
Tuduri, J., Bozkurt, E., Oguz, K., and Tokay, B.: Structural, lithological,
and geodynamic controls on geothermal activity in the Menderes geothermal
Province (Western Anatolia, Turkey), Int. J. Earth Sci., 108, 301–328,
https://doi.org/10.1007/s00531-018-1655-1, 2019.
Saar, M. O. and Manga, M.: Depth dependence of permeability in the Oregon
Cascades inferred from hydrogeologic, thermal, seismic, and magmatic
modeling constraints, J. Geophys. Res., 109, B04204, https://doi.org/10.1029/2003JB002855, 2004.
Scott, S. and Driesner, T.: Permeability changes resulting from quartz
precipitation and dissolution around upper crustal intrusions, Geofluids,
2018, 6957306, https://doi.org/10.1155/2018/6957306, 2018.
Scott, S., Driesner, T., and Weis, P.: Geologic controls on supercritical
geothermal resources above magmatic intrusions, Nat. Commun., 6, 7837,
https://doi.org/10.1038/ncomms8837, 2015.
Sibson, R. H.: Implications of fault-valve behaviour for rupture nucleation
and recurrence, Tectonophysics, 211, 283–293, https://doi.org/10.1016/0040-1951(92)90065-E, 1992.
Scibek, J.: Multidisciplinary database of permeability of fault zones and
surrounding protolith rocks at world-wide sites, Sci. Data, 7, 95,
https://doi.org/10.1038/s41597-020-0435-5, 2020.
Simms, M. A. and Garven, G.: Thermal convection in faulted extensional
sedimentary basins: theoretical results from finite-element modeling,
Geofluids, 4, 109–130, https://doi.org/10.1111/j.1468-8115.2004.00069.x, 2004.
Sonney, R. and Vuataz, F.-D.: Numerical modelling of Alpine deep flow
systems: a management and prediction tool for an exploited geothermal
reservoir (Lavey-les-Bains, Switzerland), Hydrogeol. J., 17, 601–616,
https://doi.org/10.1007/s10040-008-0394-y, 2009.
Stober, I. and Bucher, K.: Hydraulic conductivity of fractured upper crust:
insights from hydraulic tests in boreholes and fluid-rock interaction in
crystalline basement rocks, Geofluids, 15, 161–178, https://doi.org/10.1111/gfl.12104, 2015.
Sutherland, R., Townend, J., Toy, V., et al.: Extreme hydrothermal conditions at an active
plate-bounding fault, Nature, 546, 137–151, https://doi.org/10.1038/nature22355, 2017.
Taillefer, A., Soliva, R., Guillou-Frottier, L., Le Goff, E., Martin, G.,
and Seranne, M.: Fault-related controls on upward hydrothermal flow: an
integrated geological study of the Têt fault system, Eastern
Pyrénées (France), Geofluids, 2017, 8190109, https://doi.org/10.1155/2017/8190109, 2017.
Taillefer, A., Guillou-Frottier, L., Soliva, R., Magri, F., Lopez, S.,
Courrioux, G., Millot, R., Ladouche, B., and Le Goff, E.: Topographic and
faults control of hydrothermal circulation along dormant faults in an
orogen, Geochem. Geophy. Geosy, 19, 4972–4995, https://doi.org/10.1029/2018GC007965, 2018.
Tenthorey, E. and Cox, S. F.: Reaction-enhanced permeability during
serpentinite dehydration, Geology, 31, 921–924, https://doi.org/10.1130/G19724.1, 2003.
Tenthorey, E. and Fitzgerald, J. D.: Feedbacks between
deformation, hydrothermal reaction and permeability evolution in the crust:
experimental insights, Earth Planet. Sc. Lett., 247, 117–129, https://doi.org/10.1016/j.epsl.2006.05.005, 2006.
Turcotte, D. L. and Schubert, G.: Geodynamics, 2nd Edn., Cambridge
University Press, New York, 456 pp., 2002.
Violay, M., Heap, M. J., Acosta, M., and Madonna, C.: Porosity evolution at
the brittle-ductile transition in the continental crust: Implications for
deep hydrogeothermal circulation, Sci. Rep.-UK, 7, 7705, https://doi.org/10.1038/s41598-017-08108-5, 2017.
Wang, M., Kassoy, D. R., and Weidman, P. D.: Onset of convection in a
vertical slab of saturated porous media between two impermeable conducting
blocks, Int. J. Heat Mass Tran., 30, 1331–1341, https://doi.org/10.1016/0017-9310(87)90165-7, 1987.
Wanner, C., Diamond, L. W., and Alt-Epping, P.: Quantification of 3-D
thermal anomalies from surface observations of an orogenic geothermal system
(Grimsel Pass, Swiss Alps), J. Geophys. Res., 124, 10839–10854, https://doi.org/10.1029/2019JB018335 2019.
Watanabe, N., Sakagushi, K., Goto, R., Miura T., Yamane, K., Ishibaashi, T.,
Chen, Y., Komai, T., and Tsuchiya, N.: Cloud-fracture networks as a means of
accessing superhot geothermal energy, Sci. Rep.-UK, 9, 939, https://doi.org/10.1038/s41598-018-37634-z, 2019.
Weis, P., Driesner, T., and Heinrich, C. A.: Porphyry-copper ore shells form
at stable pressure-temperature fronts within dynamic fluid plumes, Science,
338, 1613–1616, https://doi.org/10.1126/science.1225009, 2012.
Weis, P., Driesner, T., Coumou, D., and Geiger, S.: Hydrothermal, multiphase
convection of H2O-NaCl fluids from ambient to magmatic temperatures: a new
numerical scheme and benchmarks for code comparison, Geofluids, 14, 347–371,
https://doi.org/10.1111/gfl.12080, 2014.
Weis, P.: The dynamic interplay between saline fluid flow and rock
permeability in magmatic-hydrothermal systems, Geofluids, 15, 350–371,
https://doi.org/10.1111/gfl.12100, 2015.
Wüstefeld, P., Hilse, U., Lüders, V., Wemmer, K., Koehrer, B., and
Hilgers, C.: Kilometer-scale fault-related thermal anomalies in tight gas
sandstones, Mar. Petroleum Geol., 86, 288–303, https://doi.org/10.1016/j.marpetgeo.2017.05.015, 2017.
Zhao, C., Hobbs, B.
E., Mühlhaus, H. B., Ord, A., and Lin, G.: Convective instability of 3-D
fluid-saturated geological fault zones heated from below, Geophys. J.
Int., 155, 213–220, https://doi.org/10.1046/j.1365-246X.2003.02032.x, 2003.
Short summary
In the first kilometers of the subsurface, temperature anomalies due to heat conduction rarely exceed 20–30°C. However, when deep hot fluids in the shallow crust flow upwards, for example through permeable fault zones, hydrothermal convection can form high-temperature geothermal reservoirs. Numerical modeling of hydrothermal convection shows that vertical fault zones may host funnel-shaped, kilometer-sized geothermal reservoirs whose exploitation would not need drilling at depths below 2–3 km.
In the first kilometers of the subsurface, temperature anomalies due to heat conduction rarely...
Special issue