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Artykuły w czasopismach na temat "Fault rheology"
Lavallée, Yan, Takehiro Hirose, Jackie E. Kendrick, Kai-Uwe Hess i Donald B. Dingwell. "Fault rheology beyond frictional melting". Proceedings of the National Academy of Sciences 112, nr 30 (29.06.2015): 9276–80. http://dx.doi.org/10.1073/pnas.1413608112.
Pełny tekst źródłaVerberne, Berend A., Oliver Plümper i Christopher J. Spiers. "Nanocrystalline Principal Slip Zones and Their Role in Controlling Crustal Fault Rheology". Minerals 9, nr 6 (28.05.2019): 328. http://dx.doi.org/10.3390/min9060328.
Pełny tekst źródłaOOHASHI, Kiyokazu, Toru TAKESHITA i Ken-ichi HIRAUCHI. "Evolution of Fault Zones and Its Rheology". Journal of Geography (Chigaku Zasshi) 129, nr 4 (25.08.2020): 473–89. http://dx.doi.org/10.5026/jgeography.129.473.
Pełny tekst źródłavan der Elst, Nicholas J., Andrew A. Delorey, David R. Shelly i Paul A. Johnson. "Fortnightly modulation of San Andreas tremor and low-frequency earthquakes". Proceedings of the National Academy of Sciences 113, nr 31 (18.07.2016): 8601–5. http://dx.doi.org/10.1073/pnas.1524316113.
Pełny tekst źródłaLiao, Chun-Fu, Strong Wen, Chau-Huei Chen i Ying-Nien Chen. "Exploring the Rheology of a Seismogenic Zone by Applying Seismic Variation". Applied Sciences 11, nr 19 (23.09.2021): 8847. http://dx.doi.org/10.3390/app11198847.
Pełny tekst źródłaAult, A. K., J. L. Jensen, R. G. McDermott, F. A. Shen i B. R. Van Devener. "Nanoscale evidence for temperature-induced transient rheology and postseismic fault healing". Geology 47, nr 12 (15.10.2019): 1203–7. http://dx.doi.org/10.1130/g46317.1.
Pełny tekst źródłaBachura, M., T. Fischer, J. Doubravová i J. Horálek. "From earthquake swarm to a main shock–aftershocks: the 2018 activity in West Bohemia/Vogtland". Geophysical Journal International 224, nr 3 (4.11.2020): 1835–48. http://dx.doi.org/10.1093/gji/ggaa523.
Pełny tekst źródłaDotseva, Zornitsa, Dian Vangelov i Ianko Gerdjikov. "The Botevgrad basin main characteristics and evolution". Geologica Balcanica 47, nr 2 (listopad 2018): 47–58. http://dx.doi.org/10.52321/geolbalc.47.2.47.
Pełny tekst źródłaHéja, Gábor Herkules, Zsolt Kercsmár, Szilvia Kövér, Tamás Budai, Mohamed Yazid Noui i László Fodor. "The Role of Rheology and Fault Geometry on Fault Reactivation: A Case-Study from the Zsámbék-Mány Basin, Central Hungary". Geosciences 12, nr 12 (24.11.2022): 433. http://dx.doi.org/10.3390/geosciences12120433.
Pełny tekst źródłaPreuss, Simon, Jean Paul Ampuero, Taras Gerya i Ylona van Dinther. "Characteristics of earthquake ruptures and dynamic off-fault deformation on propagating faults". Solid Earth 11, nr 4 (22.07.2020): 1333–60. http://dx.doi.org/10.5194/se-11-1333-2020.
Pełny tekst źródłaRozprawy doktorskie na temat "Fault rheology"
Finzi, Yaron. "Strike-slip fault structure and fault-system evolution : a numerical study applying damage rheology". Thesis, University of British Columbia, 2010. http://hdl.handle.net/2429/19401.
Pełny tekst źródłaKaneko, Yoshihiro Clayton Robert W. Lapusta Nadia. "Investigations of earthquake source processes based on fault models with variable friction rheology /". Diss., Pasadena, Calif. : California Institute of Technology, 2009. http://resolver.caltech.edu/CaltechETD:etd-04282009-202026.
Pełny tekst źródłaLindsey, Eric Ostrom. "Fault properties, rheology and interseismic deformation in Southern California from high-precision space geodesy". Thesis, University of California, San Diego, 2015. http://pqdtopen.proquest.com/#viewpdf?dispub=3721663.
Pełny tekst źródłaThis dissertation presents the collection and processing of dense high-precision geode- tic data across major faults throughout Southern California. The results are used to inform numerical models of the long-term slip rate and interseismic behavior of these faults, as well as their frictional and rheological properties at shallow depths. The data include campaign surveys of dense networks of GPS monuments crossing the faults, and Interferometric Synthetic Aperture Radar (InSAR) observations from ENVISAT. Using a Bayesian framework, we first assess to what extent these data constrain relative fault slip rates on the San Andreas and San Jacinto faults, and show that the inferred parameters depend critically on the assumed fault geometry. We next look in detail at near-field observations of strain across the San Jacinto fault, and show that the source of this strain may be either deep anomalous creep or a new form of shallow, distributed yielding in the top few kilometers of the crust. On the San Andreas fault, we show that this type of shallow yielding does occur, and its presence or absence is controlled by variations in the local normal stress that result from subtle bends in the fault. Finally, we investigate shallow creep on the Imperial fault, and show that thanks to observations from all parts of the earthquake cycle it is now possible to obtain a strong constraint on the shallow frictional rheology and depth of the material responsible for creep. The results also suggest activity on a hidden fault to the West, whose existence has been previously suggested but never confirmed.
Almeida, Jaime. "Kinematic Evolution of aTranscurrent Fault Propagating Through Consecutive Volcanic Cones:a Case of Rheology and Separation". Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-303929.
Pełny tekst źródłaO objectivo deste trabalho foi o de estabelecer os efeitos de uma única falha de desligamento direito emdois obstáculos cónicos consecutivos, de relevo positivo. Adicionalmente, procura-se estabelecer o efeito que uma camada basal dúctil poderá ter na deformação dos obstáculos.Como tal, uma série de modelos análogos foram efetuados onde dois cones de areia consecutivosforam colocados sistematicamente mais próximos um do outro. Durante estas experiências, parâmetros chave de natureza estrutural e de strain foram medidos, tais como os rácios de strain axial e angular,bem como a direção e largura das bacias formadas. Este procedimento foi repetido com uma camadabasal de silicone (PDMS) colocada por baixo dos obstáculos. Os resultados mostram que, para modelos sem a camada de silicone basal, a distância de separação dos cones tem uma influência muito forte no produto final da deformação nos cones. A proximidade dos obstáculos causa um aumento da deformação (ex. valores mais elevados de strain angular e strain axial) em ambos os obstáculos. Este efeito é particularmente visível no primeiro obstáculo, sendo este afetado por uma rotação no sentido dos ponteiros do relógio mais elevada que o segundo.Por fim, verifica-se que a presença da camada basal dúctil nulifica o efeito anterior e, quando presente, focaliza a deformação, não só criando bacias de pull-apart mais estreitas mas tambémcausando uma maior rotação nos obstáculos.
Toy, Virginia Gail, i n/a. "Rheology of the Alpine Fault Mylonite Zone : deformation processes at and below the base of the seismogenic zone in a major plate boundary structure". University of Otago. Department of Geology, 2008. http://adt.otago.ac.nz./public/adt-NZDU20080305.110949.
Pełny tekst źródłaDempsey, Edward Damien. "The kinematics, rheology, structure and anisotropy of the Alpine schist derived Alpine fault zone mylonites, New Zealand". Thesis, University of Liverpool, 2010. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.539562.
Pełny tekst źródłaBell, Marcus Antony. "The earthquake cycle of the Manyi Fault, Tibet". Thesis, University of Oxford, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.669902.
Pełny tekst źródłaShu, Weiwei. "Analogical modelling of frictional slip on faults : implications for induced and triggered seismicity". Electronic Thesis or Diss., Strasbourg, 2024. http://www.theses.fr/2024STRAH004.
Pełny tekst źródłaThe multi-scale roughness of a fault interface is responsible for multiple asperities that establish a complex and discrete set of real contacts. Since asperities control the initiation and evolution of the fault slip, it is important to explore the intrinsic relationships between the collective behavior of local asperities and the frictional stability of the global fault. Here we propose a novel analog experimental approach, which allows us to capture the temporal evolution of the slip of each asperity on a faulting interface. We find that many destabilizing events at the local asperity scale occurred in the slip-strengthening stage which is conventionally considered as the stable regime of a fault. We compute the interseismic coupling to evaluate the slipping behaviors of asperities during the slip-strengthening stage. We evidence that the interseismic coupling can be affected by the elastic interactions between asperities through the embedding soft matrix. Scaling laws of natural slow slip events are reproduced by our setup in particular the moment-duration scaling
GREFFET, PASCAL MARIE-MADELEINE. "Source sismique et endommagement : etude physique et numerique". Paris 7, 1988. http://www.theses.fr/1988PA077065.
Pełny tekst źródłaTaverna, Joël. "Modélisation mécanique des déformations de la lithosphère". Grenoble 1, 1998. http://www.theses.fr/1998GRE10084.
Pełny tekst źródłaKsiążki na temat "Fault rheology"
Bos, Bart. Faults, fluids and friction: Effect of pressure solution and phyllosilicates on fault slip behaviour, with implications for crustal rheology. [Utrecht]: Faculteit Aardwetenschappen der Universiteit Utrecht, 2000.
Znajdź pełny tekst źródłaPeter, Bird, i United States. National Aeronautics and Space Administration., red. Neotectonics of Asia: Thin-shell finite-element models with faults. [Washington, DC: National Aeronautics and Space Administration, 1994.
Znajdź pełny tekst źródłaCzęści książek na temat "Fault rheology"
Finzi, Yaron, Elizabeth H. Hearn, Yehuda Ben-Zion i Vladimir Lyakhovsky. "Structural Properties and Deformation Patterns of Evolving Strike-slip Faults: Numerical Simulations Incorporating Damage Rheology". W Mechanics, Structure and Evolution of Fault Zones, 1537–73. Basel: Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0138-2_2.
Pełny tekst źródłaWu, Patrick. "Postglacial induced surface motion, gravity and fault instability in Laurentia: Evidence for power law rheology in the mantle?" W Ice Sheets, Sea Level and the Dynamic Earth, 219–31. Washington, D. C.: American Geophysical Union, 2002. http://dx.doi.org/10.1029/gd029p0219.
Pełny tekst źródłaDragoni, M. "Crustal Deformation Due to Aseismic Slip on Buried Faults". W Glacial Isostasy, Sea-Level and Mantle Rheology, 403–23. Dordrecht: Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3374-6_20.
Pełny tekst źródła"Seismic Fault Rheology and Earthquake Dynamics". W Tectonic Faults. The MIT Press, 2007. http://dx.doi.org/10.7551/mitpress/6703.003.0007.
Pełny tekst źródła"Group Report: Rheology of Fault Rocks and Their Surroundings". W Tectonic Faults. The MIT Press, 2007. http://dx.doi.org/10.7551/mitpress/6703.003.0009.
Pełny tekst źródła"Continental Fault Structure and Rheology from the Frictional-to-Viscous Transition Downward". W Tectonic Faults. The MIT Press, 2007. http://dx.doi.org/10.7551/mitpress/6703.003.0008.
Pełny tekst źródła"9. The Strength of the San Andreas Fault: A Discussion". W Rheology and Deformation of the Lithosphere at Continental Margins, 261–83. Columbia University Press, 2004. http://dx.doi.org/10.7312/karn12738-010.
Pełny tekst źródła"8. Structure of Large-Displacement, Strike-Slip Fault Zones in the Brittle Continental Crust". W Rheology and Deformation of the Lithosphere at Continental Margins, 223–60. Columbia University Press, 2004. http://dx.doi.org/10.7312/karn12738-009.
Pełny tekst źródłaWilson, Alan J., Nick Lisowiec, Cameron Switzer, Anthony C. Harris, Robert A. Creaser i C. Mark Fanning. "Chapter 11: The Telfer Gold-Copper Deposit, Paterson Province, Western Australia". W Geology of the World’s Major Gold Deposits and Provinces, 227–49. Society of Economic Geologists, 2020. http://dx.doi.org/10.5382/sp.23.11.
Pełny tekst źródłaDavis, George H., Eytan Bos Orent, Christopher Clinkscales, Felipe R. Ferroni, George E. Gehrels, Sarah W. M. George, Katherine A. Guns i in. Structural Analysis and Chronologic Constraints on Progressive Deformation within the Rincon Mountains, Arizona: Implications for Development of Metamorphic Core Complexes. Geological Society of America, 2023. http://dx.doi.org/10.1130/2023.1222(01).
Pełny tekst źródłaStreszczenia konferencji na temat "Fault rheology"
Singleton, John, Nikki M. Seymour, Skyler Mavor, Rodrigo Gomila, Gert Heuser, Gloria Arancibia i Rachel C. Ruthven. "RHEOLOGY AND STRAIN LOCALIZATION ALONG THE INTRA-ARC ATACAMA FAULT SYSTEM, NORTHERN CHILE". W GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-382884.
Pełny tekst źródłaMcDermott, Robert, Alexis K. Ault, James P. Evans, Kelsey F. Wetzel i Fen-Ann Shen. "SPATIALLY VARIABLE COSEISMIC TEMPERATURE RISE AND TRANSIENT RHEOLOGY ALONG HEMATITE FAULT MIRRORS IN THE WASATCH FAULT ZONE, UTAH, USA". W GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-369856.
Pełny tekst źródłaSong, Won Joon, Bo Ra Song, Scott E. Johnson i Christopher C. Gerbi. "FAULT-ADJACENT DAMAGE AT THE BASE OF THE SEISMOGENIC ZONE AND IMPLICATIONS FOR CRUSTAL RHEOLOGY". W 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328698.
Pełny tekst źródłaFitzgerald, Paul G., Jeffrey A. Benowitz, Kenneth D. Ridgway, Thomas S. Warfel i Wai K. Allen. "THE ROLE OF TERRANE RHEOLOGY VS FAULT GEOMETRY FOR MOUNTAIN FORMATION AND EXHUMATION ALONG THE DENALI FAULT OF SOUTH-CENTRAL ALASKA". W GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-305797.
Pełny tekst źródłaSarkar (Mondal), Seema, i Piu Kundu. "Creeping effect of a buried, inclined, finite strike-slip fault in visco-elastic medium of Burger’s Rheology". W 2nd EAGE Conference on Reservoir Geoscience. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201977050.
Pełny tekst źródłaFitzgerald, Paul G., Thomas S. Warfel, Jeffrey A. Benowitz, Kenneth D. Ridgway, Wai K. Allen, Robert J. Gillis i Paul B. O'Sullivan. "EXHUMATION WEST OF THE EASTERN DENALI FAULT–TOTSCHUNDA FAULT “FREEWAY JUNCTION” IN SOUTH-CENTRAL ALASKA: TEMPORAL AND SPATIAL PATTERNS ADDRESSING THE RELATIVE IMPORTANCE OF TERRANE RHEOLOGY VS FAULT GEOMETRY". W GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338481.
Pełny tekst źródłaSalem, A. C., K. E. Karlstrom, M. L. Williams i D. Koning. "INSIGHTS FROM RECENT MAPPING IN THE OJO CALIENTE AND LA MADERA QUADRANGLES, TUSAS MOUNTAINS, NEW MEXICO; KINEMATICS, TIMING, AND RHEOLOGY OF PROTEROZOIC DEFORMATION AND FAULT REACTIVATION". W 2007 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2007. http://dx.doi.org/10.56577/sm-2007.2701.
Pełny tekst źródłaBorges Filho, Moacyr Nogueira, Thalles Pereira Mello, Cláudia Miriam Scheid, Luís Américo Calçada, Alex Tadeu Waldman, Gleber Teixeira i André Leibsohn Martins. "Real-Time Anomaly Detection Methodology for Drilling Fluids Properties". W SPE/IADC International Drilling Conference and Exhibition. SPE, 2023. http://dx.doi.org/10.2118/212443-ms.
Pełny tekst źródłaSullivan, Walter A. "RHEOLOGIC EVOLUTION OF A CRUSTAL-SCALE STRIKE-SLIP FAULT ZONE: A CASE STUDY OF THE KELLYLAND FAULT ZONE IN EASTERN MAINE". W 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328268.
Pełny tekst źródłaBenberber, Mohammed Rebbou, Omar Nazih, Adelson Jose Calleia de Barros, Ahmed Abdelrahim Almaazmi, Alexandre Bezerra De Melo, Mohamed Ahmed AbdelSattar, Michelle Carine Santos Rocha i in. "Innovative Approach for Lost Circulation Treatment in Surface Hole Across Naturally Fractured Limestone Formations Offshore UAE". W ADIPEC. SPE, 2022. http://dx.doi.org/10.2118/211526-ms.
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