Relevant bibliographies by topics / Fault zone

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Fault zone'

Author: Grafiati
Published: 4 June 2021
Last updated: 26 July 2025

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Journal articles on the topic "Fault zone"

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Forouzesh, Alireza, Mohammad S. Golsorkhi, Mehdi Savaghebi, and Mehdi Baharizadeh. "Support Vector Machine Based Fault Location Identification in Microgrids Using Interharmonic Injection." Energies 14, no. 8 (2021): 2317. http://dx.doi.org/10.3390/en14082317.

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This paper proposes an algorithm for detection and identification of the location of short circuit faults in islanded AC microgrids (MGs) with meshed topology. Considering the low level of fault current and dependency of the current angle on the control strategies, the legacy overcurrent protection schemes are not effective in in islanded MGs. To overcome this issue, the proposed algorithm detects faults based on the rms voltages of the distributed energy resources (DERs) by means of support vector machine classifiers. Upon detection of a fault, the DER which is electrically closest to the fau
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KOTHYARI, G. C., R. K. DUMKA, A. P. SINGH, G. CHAUHAN, M. G. THAKKAR, and S. K. BISWAS. "Tectonic evolution and stress pattern of South Wagad Fault at the Kachchh Rift Basin in western India." Geological Magazine 154, no. 4 (2016): 875–87. http://dx.doi.org/10.1017/s0016756816000509.

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AbstractWe describe a study of the E–W-trending South Wagad Fault (SWF) complex at the eastern part of the Kachchh Rift Basin (KRB) in Western India. This basin was filled during Late Cretaceous time, and is presently undergoing tectonic inversion. During the late stage of the inversion cycle, all the principal rift faults were reactivated as transpressional strike-slip faults. The SWF complex shows wrench geometry of an anastomosing en échelon fault, where contractional and extensional segments and offsets alternate along the Principal Deformation Zone (PDZ). Geometric analysis of different s
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Sexton, John L., and Harvey Henson Jr. "Interpretation of seismic reflection and gravity profile data in western Lake Superior." Canadian Journal of Earth Sciences 31, no. 4 (1994): 652–60. http://dx.doi.org/10.1139/e94-058.

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The interpretation of 1047 km of seismic reflection data collected in western Lake Superior is presented along with reflection traveltime contour maps and gravity models to understand the overall geometry of the Midcontinent Rift System beneath the lake. The Douglas, Isle Royale, and Keweenaw fault zones, clearly imaged on the seismic profiles, are interpreted to be large offset detachment faults associated with initial rifting. These faults have been reactivated as reverse faults with 3–5 km of throw. The Douglas Fault Zone is not directly connected with the Isle Royale Fault Zone. The seismi
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Onwuka, I. K., O. Oputa, G. C. Diyoke, C. S. Ezeonye, and P. I. Obi. "EFFECTS OF VARYING FAULT IMPEDANCE ON DISTANCE PROTECTION SCHEMES OF 11 KV DISTRIBUTION SYSTEMS." BAYERO JOURNAL OF ENGINEERING AND TECHNOLOGY 18, no. 2 (2023): 71–83. https://doi.org/10.5281/zenodo.14520847.

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Distance protection schemes are used in the protection of transmission and distribution lines and they use distance relay in their operations. The protection scheme is always partitioned into two or more zones and each zone is a certain percentage of the entire length of the line (which may also include the next line). With all things being equal, the tripping of the relays is solely a function of the zones where the fault occurred, that is, the location of the occurrence of the fault. However, it has been shown in this paper through simulations in Power System Computer-Aided Design (PSCAD) th
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Wang, You Xi, and Guang Zhe Deng. "Numerical Simulation of Vertical Ground Stress Distribution along Fault Trend Direction in a Metal Mine." Applied Mechanics and Materials 204-208 (October 2012): 119–22. http://dx.doi.org/10.4028/www.scientific.net/amm.204-208.119.

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The fault breaks continuous ground stress distribution. The rock mass in fault zone is weak and broken, it becomes stress decreasing zone. The paper, which is combined with engineering practice and rock mechanics test, numerically simulates geological environment of fault zones and analyzes faults trend direction influence on ground stress distribution in the metal mine. The results demonstrates that deep faults breaks down the continuity of ground stress distribution, principle stresses in lower wall of faults are smaller than it in hanging wall while high deep ground stresses are in cross di
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Kirkwood, Donna, and Michel Malo. "Across-strike geometry of the Grand Pabos fault zone: evidence for Devonian dextral transpression in the Quebec Appalachians." Canadian Journal of Earth Sciences 30, no. 7 (1993): 1363–73. http://dx.doi.org/10.1139/e93-117.

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The principal faults of southeastern Gaspé Peninsula in Quebec consist of a central high-strain zone that is characterized by mainly ductile deformation structures and bordered by low-strain zones each dominated by brittle deformation structures. The overall geometry of shear fractures within the low-strain zones is quite similar to the expected geometry of Riedel shear fractures. The brittle structures overprint the dominant C–S-type fabric of the high-strain zone, which implies that brittle deformation outlasted ductile deformation. The asymmetry of local micro- to meso-scale deformation fea
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Ichinose, Gene A., Kenneth D. Smith, and John G. Anderson. "Moment tensor solutions of the 1994 to 1996 Double Spring Flat, Nevada, earthquake sequence and implications for local tectonic models." Bulletin of the Seismological Society of America 88, no. 6 (1998): 1363–78. http://dx.doi.org/10.1785/bssa0880061363.

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Abstract The 12 September 1994 Mw 5.8 Double Spring Flat, Nevada, earthquake initiated at the intersection of a northeast- and northwest-striking set of conjugate faults within an overlapping zone between the Genoa and Antelope Valley fault zones, of the eastern Sierra Nevadan range frontal fault system. The mainshock ruptured on the northeast-striking fault plane. Eight days after the mainshock, the aftershock activity migrated from the mainshock fault plane to the northwest-striking conjugate fault. Over the next 2 years, aftershocks migrated southward onto another set of conjugate faults an
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Özsayin, Erman, and Kadir Dirik. "The role of oroclinal bending in the structural evolution of the Central Anatolian Plateau: evidence of a regional changeover from shortening to extension." Geologica Carpathica 62, no. 4 (2011): 345–59. http://dx.doi.org/10.2478/v10096-011-0026-7.

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The role of oroclinal bending in the structural evolution of the Central Anatolian Plateau: evidence of a regional changeover from shortening to extensionThe NW-SE striking extensional Inönü-Eskişehir Fault System is one of the most important active shear zones in Central Anatolia. This shear zone is comprised of semi-independent fault segments that constitute an integral array of crustal-scale faults that transverse the interior of the Anatolian plateau region. The WNW striking Eskişehir Fault Zone constitutes the western to central part of the system. Toward the southeast, this system splays
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Ma, Bingshan, Jiafu Qi, and Jiawang Ge. "Development of two-phase transfer zones during multiphase rifting and their influence on sedimentation in the Baxian Sag, Bohai Bay Basin, northern China." Geological Magazine 156, no. 11 (2019): 1821–38. http://dx.doi.org/10.1017/s0016756819000190.

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AbstractWe investigate the formation and deformation of transfer zones and their impact on sedimentation during multiphase rifting using a three-dimensional seismic dataset in the Baxian Sag, the onshore part of the Bohai Bay Basin, northern China. The fault system in the study area is dominated by two arcuate, opposing boundary faults, that is, the Niudong and Maxi faults, which form an S-type fault system which does not link together. The fault system and structural-stratigraphic features between the Eocene and Oligocene syn-rift sequences were distinctly different during the Palaeogene rift
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Fletcher, John M., Orlando J. Teran, Thomas K. Rockwell, et al. "An analysis of the factors that control fault zone architecture and the importance of fault orientation relative to regional stress." GSA Bulletin 132, no. 9-10 (2020): 2084–104. http://dx.doi.org/10.1130/b35308.1.

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Abstract The moment magnitude 7.2 El Mayor–Cucapah (EMC) earthquake of 2010 in northern Baja California, Mexico produced a cascading rupture that propagated through a geometrically diverse network of intersecting faults. These faults have been exhumed from depths of 6–10 km since the late Miocene based on low-temperature thermochronology, synkinematic alteration, and deformational fabrics. Coseismic slip of 1–6 m of the EMC event was accommodated by fault zones that displayed the full spectrum of architectural styles, from simple narrow fault zones (< 100 m in width) that have a single
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Dissertations / Theses on the topic "Fault zone"

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Watts, Lee Mark. "The Walls Boundary Fault zone and the Møre Trøndelag fault complex : a case study of two reactivated fault zones." Thesis, Durham University, 2001. http://etheses.dur.ac.uk/3878/.

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It is commonly observed that ancient faults or shear zones can become reactivated again and again, either within the same or even superimposed tectonic episodes, yet millions of years apart. Rocks of the continental crust show such effects particularly well, owing to their longevity, because through their buoyancy, continental rocks resist recycling back into the Earth's mantle over long time-scales. The Møre Trøndelag Fault Complex (MTFC), Central Norway and the Walls Boundary Fault (WBF), Shetland, were studied to elucidate the kinematic, geometric and textural evolution, in order to assess
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Najdahmadi, Seyedehbita [Verfasser]. "Imaging the North Anatolian Fault Zone with Fault Zone Head Waves, Reflected and Converted Phases / Seyedehbita Najdahmadi." Berlin : Freie Universität Berlin, 2017. http://d-nb.info/1144270219/34.

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Whitmarsh, Richard Sawyer. "Structural framework of the Fries fault zone south of Riner, Virginia." Thesis, This resource online, 1994. http://scholar.lib.vt.edu/theses/available/etd-09122009-040538/.

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Papaleo, Elvira. "The north Anatolian fault, Turkey : insights from seismic tomography." Thesis, University of Aberdeen, 2018. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=239855.

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The North Anatolian Fault Zone (NAFZ) in Turkey is a major continental strike-slip fault, 1200 km long and with a current slip rate of 25 mm/yr. Historical records show that the NAFZ is capable of producing high-magnitude earthquakes, activating different segments of the fault in a westward progression. Currently, the NAFZ poses a major seismic hazard for the city of Istanbul, which is situated close to one of the two strands into which the fault splays in northwestern Turkey. Understanding of fault zone structure and properties at depth is essential to constrain where deformation occurs withi
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Koc, Ayten. "Remote Sensing Study Of Surgu Fault Zone." Master's thesis, METU, 2005. http://etd.lib.metu.edu.tr/upload/12606611/index.pdf.

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The geometry, deformation mechanism and kinematics of the S&uuml<br>rg&uuml<br>Fault Zone is investigated by using remotely sensed data including Landsat TM and ASTER imagery combined with SRTM, and stereo-aerial photographs. They are used to extract information related to regional lineaments and tectono-morphological characteristics of the SFZ. Various image processing and enhancement techniques including contrast enhancement, PCA, DS and color composites are applied on the imagery and three different approaches including manual, semi automatic and automatic lineament extraction methods are f
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Butler, Christopher Anthony. "Basement fault reactivation : the kinematic evolution of the Outer Hebrides Fault Zone, Scotland." Thesis, Durham University, 1995. http://etheses.dur.ac.uk/1427/.

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Moir, Heather. "Modelling fault zone evolution : the effect of heterogeneity." Thesis, University of Strathclyde, 2010. http://oleg.lib.strath.ac.uk:80/R/?func=dbin-jump-full&object_id=13241.

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Dodson, Elizabeth Lauren. "STRUCTURAL GEOLOGY OF THE TRANSYLVANIA FAULT ZONE IN BEDFORD COUNTY, PENNSYLVANIA." UKnowledge, 2009. http://uknowledge.uky.edu/gradschool_theses/621.

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Transverse zones cross strike of thrust-belt structures as large-scale alignments of cross-strike structures. The Transylvania fault zone is a set of discontinuous right-lateral transverse faults striking at about 270º across Appalachian thrust-belt structures along 40º N latitude in Pennsylvania. Near Everett, Pennsylvania, the Breezewood fault terminates with the Ashcom thrust fault. The Everett Gap fault terminates westward with the Hartley thrust fault. Farther west, the Bedford fault extends westward to terminate against the Wills Mountain thrust fault. The rocks, deformed during the Alle
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Hansen, Lars. "Styles of detachment faulting at the Kane Fracture Zone oceanic core complex, 23°N Mid-Atlantic Ridge." Laramie, Wyo. : University of Wyoming, 2007. http://proquest.umi.com/pqdweb?did=1402172381&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.

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Stewart, Martyn. "Kinematic evolution of the Great Glen Fault Zone, Scotland." Thesis, Oxford Brookes University, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.364096.

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Books on the topic "Fault zone"

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Thomas, Marion Y., Thomas M. Mitchell, and Harsha S. Bhat, eds. Fault Zone Dynamic Processes. John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.

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Mancktelow, Neil S. The Simplon Fault Zone. Baumgartner, 1990.

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Senatorski, Piotr. Fault zone dynamics evolution patterns. Polska Akademia Nauk, Instytut Geofizyki, 1993.

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Eiichi, Fukuyama, and ScienceDirect (Online service), eds. Fault-Zone properties and earthquake rupture dynamics. Academic Press, 2009.

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Nelson, W. John. Ste. Genevieve fault zone, Missouri and Illinois. Division of Radiation Programs and Earth Sciences, Office of Nuclear Regulatory Research, U.S. Nuclear Regulatory Commission, 1985.

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Strehle, Barbara A. A comparison of fault zone fabrics in northwestern Vermont. Vermont Geological Survey, 1986.

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Stewart, Martyn. Kinematic evolution of the Great Glen fault zone, Scotland. Oxford Brookes University, 1997.

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G, Gass I., and Cyprus. Geological Survey Department., eds. The Geology of the southern Troodos transform fault zone. Geological Survey Department, Cyprus, 1994.

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E, Holdsworth R., ed. The nature and tectonic significance of fault zone weakening. Geological Society, 2001.

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Dubé, B. Gold metallogeny of the Cape Ray fault zone, southwestern Newfoundland. Geological Survey of Canada, 1997.

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Book chapters on the topic "Fault zone"

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van der Pluijm, Ben, and Chris Hall. "Fault Zone (Thermochronology)." In Encyclopedia of Scientific Dating Methods. Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-6326-5_250-1.

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van der Pluijm, Ben, and Chris Hall. "Fault Zone (Thermochronology)." In Encyclopedia of Scientific Dating Methods. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6304-3_250.

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Whearty, James J., Thomas K. Rockwell, and Gary H. Girty. "Incipient Pulverization at Shallow Burial Depths Along the San Jacinto Fault, Southern California." In Fault Zone Dynamic Processes. John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch1.

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Renard, François, and Thibault Candela. "Scaling of Fault Roughness and Implications for Earthquake Mechanics." In Fault Zone Dynamic Processes. John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch10.

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Klinger, Yann, Jin-Hyuck Choi, and Amaury Vallage. "Fault Branching and Long-Term Earthquake Rupture Scenario for Strike-Slip Earthquakes." In Fault Zone Dynamic Processes. John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch11.

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Passelègue, François X., Soumaya Latour, Alexandre Schubnel, Stefan Nielsen, Harsha S. Bhat, and Raúl Madariaga. "Influence of Fault Strength on Precursory Processes During Laboratory Earthquakes." In Fault Zone Dynamic Processes. John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch12.

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Ampuero, Jean Paul, and Xiaolin Mao. "Upper Limit on Damage Zone Thickness Controlled by Seismogenic Depth." In Fault Zone Dynamic Processes. John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch13.

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Thomas, Marion Y., Harsha S. Bhat, and Yann Klinger. "Effect of Brittle Off-Fault Damage on Earthquake Rupture Dynamics." In Fault Zone Dynamic Processes. John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch14.

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Korren, Caitlyn S., Eric C. Ferre, En-Chao Yeh, Yu-Min Chou, and Hao-Tsu Chu. "Seismic Rupture Parameters Deduced From a Pliocene-Pleistocene Fault Pseudotachylyte in Taiwan." In Fault Zone Dynamic Processes. John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch2.

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Mitchell, Thomas M., Jose M. Cembrano, Kazuna Fujita, et al. "Fluid Inclusion Evidence of Coseismic Fluid Flow Induced by Dynamic Rupture." In Fault Zone Dynamic Processes. John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch3.

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Conference papers on the topic "Fault zone"

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Tanaka, Izumi, Yoshinori Uchida, Kouki Ikeuchi, Kenichi Nakatsumi, Masaya Kawane, and Kenta Kobira. "Creative Seismic Design and Application of Precast Concrete Member of Nakatsugawa Bridge Over the Fault Fracture Zone - Butterfly Webs Extradosed Bridge -." In IABSE Symposium, Tokyo 2025: Environmentally Friendly Technologies and Structures: Focusing on Sustainable Approaches. International Association for Bridge and Structural Engineering (IABSE), 2025. https://doi.org/10.2749/tokyo.2025.1512.

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&lt;p&gt;The bridge is a triple-span extradosed partially prestressed concrete (PPC)bridge in a steep ravine which is located between tunnels. According to a detailed geological survey, fault fracture zones are widely spread under the bridge. Because the faults are possibility large displacement, it is designed as an extradosed bridge to prevent collapse and unrepairable damage in case of a huge earthquake.&lt;/p&gt;&lt;p&gt;Piers and towers should not be arranged near these faults, as a result, the span distribution of the bridge became unbalanced. Therefore, lightweight concrete precast pane
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Mohamed, 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.

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Analogue outcrops can be used to prepare geoscientists with realistic expectations and responses for Geosteering ultra-long horizontal wells (ERD) in thin reservoirs with different scales of faults, and uncertainty in fault zone parameters and characteristics. Geosteering ultra-long horizontal wells in specific, thin, meter-thick target zones within reservoirs is challenged when sub-seismic faults are present or where seismic scale fault throw and fault location is ill-defined or imprecisely known. This paper defines the challenge of how analogue outcrops can be used to prepare geoscientists w
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Childs, C. J., T. Manzocchi, J. J. Walsh, and M. P. J. Schopfer. "Fault Core/damage Zone; an Unhelpful Description of Fault Zone Structure?" In 3rd EAGE International Conference on Fault and Top Seals. EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20143012.

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Dias, F. C., R. Quevedo, D. Roehl, and B. Carvalho. "Assessment of Geomechanical Properties of Fault Damage Zones Based on Numerical Modeling." In 58th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2024. http://dx.doi.org/10.56952/arma-2024-1076.

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ABSTRACT: Fault zones are generally made of highly deformed rocks composed of a core surrounded by a damage zone. The core is usually formed of an impermeable consolidated material responsible for reservoir compartmentalization. However, the complex architecture of damage zones induces a substantial variability of their properties that can significantly influence fluid flow and geomechanical behavior of oil and gas fields. Therefore, characterizing damage zone properties is relevant during reservoir development, production, and management. Many studies have been carried out to characterize and
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Karasaki, Kenzi, Celia Tiemi Onishi, Erika Gasperikova, et al. "Development of Characterization Technology for Fault Zone Hydrology." In ASME 2010 13th International Conference on Environmental Remediation and Radioactive Waste Management. ASMEDC, 2010. http://dx.doi.org/10.1115/icem2010-40121.

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Several deep trenches were cut, and a number of geophysical surveys were conducted across the Wildcat Fault in the hills east of Berkeley, California. The Wildcat Fault is believed to be a strike-slip fault and a member of the Hayward Fault System, with over 10 km of displacement. So far, three boreholes of ∼ 150m deep have been core-drilled and borehole geophysical logs were conducted. The rocks are extensively sheared and fractured; gouges were observed at several depths and a thick cataclasitic zone was also observed. While confirming some earlier, published conclusions from shallow observa
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Santiago Ortega, Javier, and Maria Cristina Tavares. "Fault Impedance Analysis in Half-Wavelength Transmission Lines." In Simpósio Brasileiro de Sistemas Elétricos - SBSE2020. sbabra, 2020. http://dx.doi.org/10.48011/sbse.v1i1.2473.

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Half-wavelength (HWL) line has excellent steady-state properties to power transmission over very long distances, and technical and economic advantages over HVDC very long lines. However, protection system based on impedance calculations need carefully attention due to specific behavior of HWL line under fault. This paper analyzes the fault impedance on HLW lines to produce more insight about the effect of the capacitance, the point of fault, the resonance phenomenon, the transmission line model and the phasor estimation to the impedance measurement process in protective devices. This paper sho
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Zhang, Yu, Honglin Xiao, XiaoMing Zhang, et al. "Integration Applications of Image and Sonic Data in the Fault-Dominated Carbonate Reservoir in Tarim Basin." In Abu Dhabi International Petroleum Exhibition & Conference. SPE, 2021. http://dx.doi.org/10.2118/207427-ms.

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Abstract Carbonate reservoir is one of the most complex and important reservoirs in the world. It was confirmed that the slip-strike fault played a crucial role in the fault-dominated carbonate reservoir in Tarim basin. It is challenging to evaluate this kind of reservoir using the open-hole log or seismic data. Identifying and characterizing the fault-dominated carbonate reservoir were the objectives of this case study. High-definition borehole resistivity image and dipole sonic logs were run in several wells in the research area. It was revealed the detail features of the fault-dominated car
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Ryter, Lila. "Fault-tip damage zone development during normal fault propagation within the Sevier Fault Zone, southern Utah." In Proceedings of the Keck Geology Consortium. Keck Geology Consortium, 2025. https://doi.org/10.18277/akrsg.2025.37.06.

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Noufal, Abdelwahab. "Fault Planes Materials Fill Characteristics, UAE." In Abu Dhabi International Petroleum Exhibition & Conference. SPE, 2021. http://dx.doi.org/10.2118/207217-ms.

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Abstract Abu Dhabi subsurface fault populations triggered basin system in diverse directions, because of their significant role as fluid pathways. Studying fault infill materials, fault geometries, zone architecture and sealing properties from outcrops as analogues to the subsurface of Abu Dhabi, and combining these with well data and cores are the main objectives of this paper. The fault core around the fault plane and in areas of overlap between fault segments and around the fault tip include slip surfaces and deformed rocks such as fault gouge, breccia, and lenses of host rock, shale smear,
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Chan, A. W., D. Murray, S. De Gennaro, and G. O’Reilly. "Can Lost Circulation Materials (LCM) Cure Losses Across Fault Damage Zone?" In 57th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2023. http://dx.doi.org/10.56952/arma-2023-0478.

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ABSTRACT Severe lost circulation events have been observed from various assets across our global portfolio while drilling and completing through fault damage zones in recent years. Common characteristics of these events include: (1) pressures at which losses occurred in the proximity of fault zones appear to be significantly lower than the estimated lost circulation threshold (or fracture gradient, FG) for tensile failure of the intact formation; (2) most of these lost circulation events are dynamic in nature; (3) the more severe loss events happened when crossing fault damage zones in the mor
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Reports on the topic "Fault zone"

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Hylland, Michael D., Adam I. Hiscock, Greg N. McDonald, et al. Paleoseismic Investigation of the Taylorsville Fault at the Airport East Site, West Valley Fault Zone, Salt Lake County, Utah. Utah Geological Survey, 2022. http://dx.doi.org/10.34191/ss-169.

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The West Valley fault zone (WVFZ) and Salt Lake City segment (SLCS) of the Wasatch fault zone comprise Holoceneactive normal faults that bound an intrabasin graben in northern Salt Lake Valley, Utah. Both fault zones have evidence of recurrent Holocene surface-faulting earthquakes. A topic of recent research is the seismogenic relation of the antithetic (subsidiary) WVFZ to the Wasatch fault zone—specifically, to what degree are WVFZ earthquakes independent of slip on the SLCS, or other adjacent segments, of the Wasatch fault zone. To improve paleoseismic data for the WVFZ and better understan
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Hylland, Michael D., Adam I. Hiscock, Greg N. McDonald, et al. Paleoseismic Investigation of the Taylorsville Fault at the Airport East Site, West Valley Fault Zone, Salt Lake County, Utah. Utah Geological Survey, 2022. http://dx.doi.org/10.34191/ss-169.

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The West Valley fault zone (WVFZ) and Salt Lake City segment (SLCS) of the Wasatch fault zone comprise Holoceneactive normal faults that bound an intrabasin graben in northern Salt Lake Valley, Utah. Both fault zones have evidence of recurrent Holocene surface-faulting earthquakes. A topic of recent research is the seismogenic relation of the antithetic (subsidiary) WVFZ to the Wasatch fault zone—specifically, to what degree are WVFZ earthquakes independent of slip on the SLCS, or other adjacent segments, of the Wasatch fault zone. To improve paleoseismic data for the WVFZ and better understan
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3

Hiscock, Adam I. Hiscock, Emily J. Kleber, Susanne U. Jänecke, Greg N. McDonald, Robert Q. Oaks Jr., and Tammy Rittenour. Fault Trace Mapping and Surface-Fault-Rupture Special Study Zone Delineation of the East and West Cache Fault Zones and Other Regional Faults, Utah. Utah Geological Survey, 2024. http://dx.doi.org/10.34191/ri-286.

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The Cache Valley region in northern Utah and southern Idaho contains and is surrounded by several large, hazardous faults which pose significant earthquake risk. The 40-mile-long (65 km) East Cache fault zone (ECFZ) and the 35-mile-long (56 km) West Cache fault zone (WCFZ) bound the Cache Valley graben and both show evidence of large surface-faulting earthquakes in the late Quaternary. Other hazardous faults in the Cache Valley region include the intrabasin Dayton-Oxford fault, the Mantua area faults within the Wellsville Mountains, and the James Peak fault at the very southern end of the ECFZ
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4

Hadlari, T., R. A. Millar, and L. S. Lane. The Eskimo Lakes Fault Zone renamed Husky Lakes Fault Zone, Tuktoyaktuk Peninsula, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2020. http://dx.doi.org/10.4095/326948.

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McDonald, Greg N., Emily J. Kleber, Adam I. Hiscock, Scott E. K. Bennett, and Steve D. Bowman. Fault Trace Mapping and Surface-Fault-Rupture Special Study Zone Delineation of the Wasatch Fault Zone, Utah and Idaho. Utah Geological Survey, 2020. http://dx.doi.org/10.34191/ri-280.

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6

Dubé, B., and K. Lauzière. Cape Ray Fault Zone, SW Newfoundland. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/207599.

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Arnold, Bill Walter, Barry L. Roberts, Sean Andrew McKenna, and Timothy C. Coburn. Spatial analysis of hypocenter to fault relationships for determining fault process zone width in Japan. Office of Scientific and Technical Information (OSTI), 2004. http://dx.doi.org/10.2172/876371.

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Dube, B., K. Lauziere, and A. Tremblay. Structural geology of a crustal scale fault zone: the Cape Ray Fault coastal section, southwestern Newfoundland. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/132896.

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Dubé, B., and K. Lauzière. Gold metallogeny of the Cape Ray Fault Zone, southwest Newfoundland. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/209256.

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RIENÄCKER, Julia, Ronny LÄHNE, Wolfgang GOSSEL, and Peter WYCISK. Geological 3D model of Halle/Saale – complex fault-zone modelling (Germany). Cogeo@oeaw-giscience, 2011. http://dx.doi.org/10.5242/iamg.2011.0118.

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