Academic literature on the topic 'Fault damage zones'
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Journal articles on the topic "Fault damage zones"
Lyu, Wenya, Lianbo Zeng, Zonghu Liao, Yuanyuan Ji, Peng Lyu, and Shaoqun Dong. "Fault damage zone characterization in tight-oil sandstones of the Upper Triassic Yanchang Formation in the southwest Ordos Basin, China: Integrating cores, image logs, and conventional logs." Interpretation 5, no. 4 (November 30, 2017): SP27—SP39. http://dx.doi.org/10.1190/int-2016-0231.1.
Full textKim, Young-Seog, David C. P. Peacock, and David J. Sanderson. "Fault damage zones." Journal of Structural Geology 26, no. 3 (March 2004): 503–17. http://dx.doi.org/10.1016/j.jsg.2003.08.002.
Full textLiao, Zonghu, Luyao Hu, Xiaodi Huang, Brett M. Carpenter, Kurt J. Marfurt, Saiyyna Vasileva, and Yun Zhou. "Characterizing damage zones of normal faults using seismic variance in the Wangxuzhuang oilfield, China." Interpretation 8, no. 4 (June 30, 2020): SP53—SP60. http://dx.doi.org/10.1190/int-2020-0004.1.
Full textMa, Yuchuan, Guangcai Wang, Rui Yan, Bo Wang, Huaizhong Yu, Chen Yu, Chong Yue, and Yali Wang. "Relationship between Earthquake-Induced Hydrologic Changes and Faults." Water 13, no. 19 (October 8, 2021): 2795. http://dx.doi.org/10.3390/w13192795.
Full textLiao, Zonghu, Wei Li, Huayao Zou, Fang Hao, Kurt J. Marfurt, and Ze'ev Reches. "Composite damage zones in the subsurface." Geophysical Journal International 222, no. 1 (April 11, 2020): 225–30. http://dx.doi.org/10.1093/gji/ggaa158.
Full textZhao, Zhan, Jingtao Liu, Wenlong Ding, Ruiqiang Yang, and Gang Zhao. "Analysis of Seismic Damage Zones: A Case Study of the Ordovician Formation in the Shunbei 5 Fault Zone, Tarim Basin, China." Journal of Marine Science and Engineering 9, no. 6 (June 6, 2021): 630. http://dx.doi.org/10.3390/jmse9060630.
Full textChen, Yangpu, Zonghu Liao, Li-Yun Fu, Gang Zhou, Liang Xu, Kurt J. Marfurt, Xinru Mu, and Huayao Zou. "Effect of main frequencies on characterizing fault damage zones using forward modeling and attribute of variance." Interpretation 8, no. 4 (October 12, 2020): SP157—SP165. http://dx.doi.org/10.1190/int-2020-0017.1.
Full textBloom, Colin K., Andrew Howell, Timothy Stahl, Chris Massey, and Corinne Singeisen. "The influence of off-fault deformation zones on the near-fault distribution of coseismic landslides." Geology 50, no. 3 (November 22, 2021): 272–77. http://dx.doi.org/10.1130/g49429.1.
Full textPaul, Pijush K., Mark D. Zoback, and Peter H. Hennings. "Fluid Flow in a Fractured Reservoir Using a Geomechanically Constrained Fault-Zone-Damage Model for Reservoir Simulation." SPE Reservoir Evaluation & Engineering 12, no. 04 (July 6, 2009): 562–75. http://dx.doi.org/10.2118/110542-pa.
Full textTorabi, A., T. S. S. Ellingsen, M. U. Johannessen, B. Alaei, A. Rotevatn, and D. Chiarella. "Fault zone architecture and its scaling laws: where does the damage zone start and stop?" Geological Society, London, Special Publications 496, no. 1 (August 7, 2019): 99–124. http://dx.doi.org/10.1144/sp496-2018-151.
Full textDissertations / Theses on the topic "Fault damage zones"
Mitchell, Thomas Matthew. "The fluid flow properties of fault damage zones." Thesis, University of Liverpool, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.485852.
Full textSeverin, Jordan Melvin. "Impact of faults and fault damage zones on large open pit slopes." Thesis, University of British Columbia, 2017. http://hdl.handle.net/2429/61064.
Full textScience, Faculty of
Earth, Ocean and Atmospheric Sciences, Department of
Graduate
Aben, Frans. "Experimental simulation of the seismic cycle in fault damage zones." Thesis, Université Grenoble Alpes (ComUE), 2016. http://www.theses.fr/2016GREAU012/document.
Full textEarthquakes along large crustal scale faults are a huge hazard threatening large populations. The behavior of such faults is influenced by the fault damage zone that surrounds the fault core. Fracture damage in such fault damage zones influences each stage of the seismic cycle. The damage zone influences rupture mechanics, behaves as a fluid conduit to release pressurized fluids at depth or to give access to reactive fluids to alter the fault core, and facilitates strain during post- and interseismic periods. Also, it acts as an energy sink for earthquake energy. Here, laboratory experiments were performed to come to a better understanding of how this fracture damage is formed during coseismic transient loading, what this fracture damage can tell us about the earthquake rupture conditions along large faults, and how fracture damage is annihilated over time.First, coseismic damage generation, and specifically the formation of pulverized fault damage zone rock, is reviewed. The potential of these pulverized rocks as a coseismic marker for rupture mechanisms is discussed. Although these rocks are promising in that aspect, several open questions remain.One of these open questions is if the transient loading conditions needed for pulverization can be reduced by progressively damaging during many seismic events. The successive high strain rate loadings performed on quartz monzonites using a split Hopkinson pressure bar reveal that indeed the pulverization strain rate threshold is reduced by at least 50%.Another open question is why pulverized rocks are almost always observed in crystalline lithologies and not in more porous rock, even when crystalline and porous rocks are juxtaposed by a fault. To study this observation, high strain rate experiments were performed on porous Rothbach sandstone. The results show that pervasive pulverization below the grain scale, such as observed in crystalline rock, does not occur in the sandstone samples for the explored strain rate range (60-150 s-1). Damage is mainly occurs at a scale superior to that of the scale of the grains, with intragranular deformation occurring only in weaker regions where compaction bands are formed. The competition between inter- and intragranular damage during dynamic loading is explained with the geometric parameters of the rock in combination with two classic micromechanical models: the Hertzian contact model and the pore-emanated crack model. In conclusion, the observed microstructures can form in both quasi-static and dynamic loading regimes. Therefore caution is advised when interpreting the mechanism responsible for near-fault damage in sedimentary rock near the surface. Moreover, the results suggest that different responses of different lithologies to transient loading are responsible for sub-surface damage zone asymmetry.Finally, post-seismic annihilation of coseismic damage by calcite assisted fracture sealing has been studied in experiments, so that the coupling between strengthening and permeability of the fracture network could be studied. A sample-scale fracture network was introduced in quartz monzonite samples, followed exposure to upper crustal conditions and percolation of a fluid saturated with calcite for several months. A large recovery of up to 50% of the initial P-wave velocity drop has been observed after the sealing experiment. In contrast, the permeability remained more or less constant for the duration of the experiment. This lack of coupling between strengthening and permeability in the first stages of sealing is explained by X-ray computed micro tomography. Incipient sealing in the fracture spaces occurs downstream of flow barriers, thus in regions that do not affect the main fluid flow pathways. The decoupling of strength recovery and permeability suggests that shallow fault damage zones can remain fluid conduits for years after a seismic event, leading to significant transformations of the core and the damage zone of faults with time
Wood, Rebekah Erin. "Fault and Fluid Interactions in the Elsinore Fault-West Salton Detachment Fault Damage Zones, Agua Caliente County Park, California." DigitalCommons@USU, 2014. https://digitalcommons.usu.edu/etd/2103.
Full textMichie, Emma A. H. "The influence of damage on the petrophysical properties of carbonate-hosted fault zones." Thesis, University of Aberdeen, 2015. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=227220.
Full textWu, Chunquan. "Fault zone damage, nonlinear site response, and dynamic triggering associated with seismic waves." Diss., Georgia Institute of Technology, 2011. http://hdl.handle.net/1853/41143.
Full textIsaacs, Angela J. "Characterizing Deformation, Damage Parameters, and Clay Composition in Fault Zones: Insights from the Chelungpu Thrust, Taiwan, and Mozumi Right Lateral Fault, Japan." DigitalCommons@USU, 2005. https://digitalcommons.usu.edu/etd/6059.
Full textNishiwaki, Takafumi. "Comparison of Damage Zones of the Nojima and the Asano Faults from the Deep Drilling Project: Differences in Meso-to-microscale Deformation Structures related to Fault Activity." Kyoto University, 2020. http://hdl.handle.net/2433/253096.
Full textDutson, Sarah J. "Effects of Hurricane Fault Architecture on Groundwater Flow in the Timpoweap Canyon of Southwestern, Utah." Diss., CLICK HERE for online access, 2005. http://contentdm.lib.byu.edu/ETD/image/etd923.pdf.
Full textMayolle, Sylvain. "Croissance des zones d’endommagement de faille : étude structurale en milieu carbonaté et modélisations analogiques." Thesis, Montpellier, 2021. http://www.theses.fr/2021MONTG019.
Full textThe study of faults in the upper crust generates interest in modeling their impact on fluid flow and the mechanical behavior of the earth's crust. Fault damage zones are important structures with multiple implications for resource management and earthquake studies. This thesis aims to characterize the distribution and growth of damage around faults and to study its impact on the Displacement - Damage thickness (D-T) scaling law. Two complementary approaches of field measurements and analog modeling of normal faults are developed to answer this question. This manuscript presents new results of fault damage mapping, D-T scaling in carbonate rocks, and the first analog modeling experiments of fault damage zones. The results show a heterogeneous and asymmetric distribution of damage around faults, mainly influenced by fault interactions during their growth (segmentation, conjugate faults). A D-T law specific to wall damage is established and shows a normal correlation between D and T for less than 100 m of fault displacement, and also confirms the existence of a damage thickness threshold after 100 m of displacement. To explain this law, we propose a damage zone growth model controlled by the interaction and coalescence of fault segments. Analog modeling experiments allowed the description of two new types of damage (graben damage and dip-change link damage), and show a failure mode transition during fault growth, from a segmented dilatational-shear mode to a localized compactional-shear mode. They also demonstrate that initiation of segmentation, segment activity selection, interaction and coalescence processes control the development of fault damage zones and the D-T law. We propose that the thickness of the faulted brittle layer is a main controlling parameter of segmentation, strain localization, and the fault damage thickness threshold observed
Book chapters on the topic "Fault damage zones"
Aben, Franciscus M., Mai-Linh Doan, Jean-Pierre Gratier, and François Renard. "Coseismic Damage Generation and Pulverization in Fault Zones." In Fault Zone Dynamic Processes, 47–80. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch4.
Full textDieterich, James H., and Deborah Elaine Smith. "Nonplanar Faults: Mechanics of Slip and Off-fault Damage." In Mechanics, Structure and Evolution of Fault Zones, 1799–815. Basel: Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0138-2_12.
Full textDor, Ory, Judith S. Chester, Yehuda Ben-Zion, James N. Brune, and Thomas K. Rockwell. "Characterization of Damage in Sandstones along the Mojave Section of the San Andreas Fault: Implications for the Shallow Extent of Damage Generation." In Mechanics, Structure and Evolution of Fault Zones, 1747–73. Basel: Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0138-2_10.
Full textSammis, Charles G., Ares J. Rosakis, and Harsha S. Bhat. "Effects of Off-fault Damage on Earthquake Rupture Propagation: Experimental Studies." In Mechanics, Structure and Evolution of Fault Zones, 1629–48. Basel: Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0138-2_5.
Full textGriffith, W. Ashley, Pablo F. Sanz, and David D. Pollard. "Influence of Outcrop Scale Fractures on the Effective Stiffness of Fault Damage Zone Rocks." In Mechanics, Structure and Evolution of Fault Zones, 1595–627. Basel: Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0138-2_4.
Full textFinzi, Yaron, Elizabeth H. Hearn, Yehuda Ben-Zion, and Vladimir Lyakhovsky. "Structural Properties and Deformation Patterns of Evolving Strike-slip Faults: Numerical Simulations Incorporating Damage Rheology." In 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.
Full textLockner, David A., Hidemi Tanaka, Hisao Ito, Ryuji Ikeda, Kentaro Omura, and Hisanobu Naka. "Geometry of the Nojima Fault at Nojima-Hirabayashi, Japan — I. A Simple Damage Structure Inferred from Borehole Core Permeability." In Mechanics, Structure and Evolution of Fault Zones, 1649–67. Basel: Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0138-2_6.
Full textNguyen, Trung Kien, Jeremy Rohmer, and Ba Thao Vu. "Influence of heterogeneous fractured fault damage zones on shear failure onset during fluid injection." In Lecture Notes in Civil Engineering, 721–26. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-15-0802-8_114.
Full textIwata, N., Y. Ohtsuka, Ö. Aydan, T. Ito, A. Sainoki, and T. Ikeda. "Analytical study on the effect of damage zones on the occurrence of surface rupture at the Hinagu fault." In Rock Dynamics: Progress and Prospect, Volume 1, 109–14. London: CRC Press, 2022. http://dx.doi.org/10.1201/9781003359142-14.
Full textAmpuero, Jean Paul, and Xiaolin Mao. "Upper Limit on Damage Zone Thickness Controlled by Seismogenic Depth." In Fault Zone Dynamic Processes, 243–53. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch13.
Full textConference papers on the topic "Fault damage zones"
Lisitsa, V., V. Tcheverda, D. Kolyukhin, and V. Volianskaia. "Simulation of Near-fault Damage Zones." In Petroleum Geostatistics 2019. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201902220.
Full textWolf, D. E., J. G. Solum, J. P. Brandenburg, and S. J. Naruk. "Quantifying the Impact of Fault Damage Zones on Reservoir Performance." In 3rd EAGE International Conference on Fault and Top Seals. Netherlands: EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20143027.
Full textMohamed, Emad AbdelAziz, and Henry Ewart Edwards. "Capturing Fault Effects in Thin Reservoirs for Geosteering Improvements in Developing Offshore Carbonate Fields." In Abu Dhabi International Petroleum Exhibition & Conference. SPE, 2021. http://dx.doi.org/10.2118/208160-ms.
Full textVaszi, A. Z., S. D. Harris, and R. J. Knipe. "3D Upscaling of Fault Damage Zones for Reservoir Modelling." In ECMOR IX - 9th European Conference on the Mathematics of Oil Recovery. European Association of Geoscientists & Engineers, 2004. http://dx.doi.org/10.3997/2214-4609-pdb.9.a016.
Full textMayolle, S., R. Soliva, Y. Caniven, C. Wibberley, G. Ballas, S. Dominguez, and G. Milési. "Scaling of Fault Damage Zones and Implications for Naturally Fractured Reservoirs." In Fifth International Conference on Fault and Top Seals. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201902342.
Full textSyngaevsky, Pavel E. "Tectonic and Overpressured Zones, Gulf of Mexico." In ASME 2001 Engineering Technology Conference on Energy. American Society of Mechanical Engineers, 2001. http://dx.doi.org/10.1115/etce2001-17172.
Full textLewis, H., A. Paez, J. Ma, and G. D. Couples. "Emergent Distributions of Stress and Strain in Fault Damage Zones." In 2nd EAGE International Conference on Fault and Top Seals - From Pore to Basin Scale 2009. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609.20147178.
Full textKolyukhin, D., and J. Tveranger. "Statistical Modelling of Fault Core and Deformation Band Structure in Fault Damage Zones." In 77th EAGE Conference and Exhibition 2015. Netherlands: EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201413043.
Full textSurpless, Benjamin, and Caroline McKeighan. "DYNAMIC FRACTURING IN FAULT TIP DAMAGE ZONES? AN OUTCROP STUDY OF THE SEVIER FAULT ZONE, SOUTHERN UTAH." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-377982.
Full textEdwards, P., D. J. Sanderson, and Y. S. Kim. "Permeability Heterogeneity in Fault Damage Zones and Its Relationship to Deformation Band Connectivity." In Fourth International Conference on Fault and Top Seals. Netherlands: EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201414061.
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