Relevant bibliographies by topics / Strike slip fault zone

Contents

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

Academic literature on the topic 'Strike slip fault zone'

Author: Grafiati
Published: 4 June 2021
Last updated: 8 February 2022

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Journal articles on the topic "Strike slip fault zone"

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Johnson, Jeffrey A. "Off-fault Deformation Associated with Strike-slip Faults." Environmental and Engineering Geoscience 24, no. 4 (2018): 375–84. http://dx.doi.org/10.2113/eeg-2030.

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Abstract Habitable buildings can be protected from surface fault rupture by establishing structure “setback zones” similar in purpose to legally mandated zones in California and Utah. But post-earthquake surveys of offset and warped linear cultural features, believed to have been straight prior to the event, demonstrate that potentially damaging inelastic strains or off-fault deformation can extend tens of meters beyond the principal slip zone of strike-slip surface fault ruptures. Setback zones designed to also mitigate off-fault deformation are likely to be prohibitively wide, indicating the
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Catalán Ormeño, Nicole Stephanie, Klaus Bataille, Andrés Tassara, and Rodolfo Araya. "Depth-dependent geometry of margin-parallel strike-slip faults within oblique subduction zones." Andean Geology 44, no. 1 (2017): 79. http://dx.doi.org/10.5027/andgeov44n1-a05.

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Based on the principle that faults develop where shear stress is maximum, we determine the depth-dependent geometry of margin-parallel strike-slip faults within oblique subduction zones. Using an elastic half-space model for the south Chile subduction zone, we show that the geometry of a margin-parallel strike-slip fault as the Liquiñe-Ofqui Fault Zone (LOFZ), is vertical near the free surface and curved downwards, until reaching the subducting slab. This geometry is compatible with the observations of reflectors on seismic data obtained from wide angle refraction studies in southern Chile. GP
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ALEKSANDROWSKI, P., R. KRYZA, S. MAZUR, and J. ŻABA. "Kinematic data on major Variscan strike-slip faults and shear zones in the Polish Sudetes, northeast Bohemian Massif." Geological Magazine 134, no. 5 (1997): 727–39. http://dx.doi.org/10.1017/s0016756897007590.

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The still highly disputable terrane boundaries in the Sudetic segment of the Variscan belt mostly seem to follow major strike-slip faults and shear zones. Their kinematics, expected to place important constraints on the regional structural models, is discussed in some detail. The most conspicuous is the WNW–ESE Intra-Sudetic Fault Zone, separating several different structural units of the West Sudetes. It showed ductile dextral activity and, probably, displacement magnitude of the order of tens to hundreds kilometres, during late Devonian(?) to early Carboniferous times. In the late Carbonifer
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Reid, L. F., P. S. Simony, and G. M. Ross. "Dextral strike-slip faulting in the Cariboo Mountains, British Columbia: a natural example of wrench tectonics in relation to Cordilleran tectonics." Canadian Journal of Earth Sciences 39, no. 6 (2002): 953–70. http://dx.doi.org/10.1139/e02-017.

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The Cariboo Mountains, British Columbia, contain an intracontinental dextral strike-slip fault system that crosscuts the regional fold structures. This fault system accounts for a minimum of 120 km and a maximum of 200 km of dextral strike-slip displacement. This probably accommodates some of the motion associated with the southern termination of the Northern Rocky Mountain Trench Fault and is part of a step-over zone between the Northern Rocky Mountain Trench Fault and the Fraser River – Straight Creek fault systems. The Isaac Lake Synclinorium is a kilometre-scale Jurassic fold structure tha
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Konon, Andrzej, Szymon Ostrowski, Barbara Rybak-Ostrowska, et al. "Mnin restraining stepover – evidence of significant Cretaceous–Cenozoic dextral strike-slip faulting along the Teisseyre-Tornquist Zone?" Acta Geologica Polonica 66, no. 3 (2016): 435–55. http://dx.doi.org/10.1515/agp-2016-0019.

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Abstract A newly recognized Mnin restraining stepover is identified in the Permo-Mesozoic cover of the western part of the Late Palaeozoic Holy Cross Mountains Fold Belt (Poland), within a fault pattern consisting of dextral strike-slip faults. The formation of a large contractional structure at the Late Cretaceous – Cenozoic transition displays the significant role of strike-slip faulting along the western border of the Teisseyre-Tornquist Zone, in the foreland of the Polish part of the Carpathian Orogen. Theoretical relationships between the maximum fault offsets/ mean step length, as well a
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Huang, Lei, Chi-yang Liu, Jun-feng Zhao, and Dong-dong Zhang. "Synrift basin inversion: Significant role of synchronous strike-slip motion in a rift basin." GSA Bulletin 132, no. 11-12 (2020): 2572–86. http://dx.doi.org/10.1130/b35435.1.

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Abstract In rift basins with superposed strike-slip deformation, the structural style of wrench elements and the roles they play in synrift architecture and evolution are important, poorly understood issues for basin analysis and hydrocarbon exploration. The NE-SW–striking Tan-Lu fault zone, located in eastern China, runs through the Liaodong Bay subbasin within the Cenozoic Bohai Bay Basin and experienced dextral strike-slip motion during the later synrift stage of the basin (ca. 40 Ma to 23 Ma). Investigations of the Liaodong Bay subbasin indicate that rift-fault reactivation and wrench-faul
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Kearse, Jesse, Yoshihiro Kaneko, Tim Little, and Russ Van Dissen. "Curved slickenlines preserve direction of rupture propagation." Geology 47, no. 9 (2019): 838–42. http://dx.doi.org/10.1130/g46563.1.

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Abstract Slip-parallel grooves (striations) on fault surfaces are considered a robust indicator of fault slip direction, yet their potential for recording aspects of earthquake rupture dynamics has received little attention. During the 2016 Kaikōura earthquake (South Island, New Zealand), >10 m of dextral strike-slip on the steeply dipping Kekerengu fault exhumed >200 m2 of fresh fault exposure (free faces) where it crossed bedrock canyons. Inscribed upon these surfaces, we observed individual striae up to 6 m long, all of which had formed during the earthquake. These were typically curv
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Little, T. A., P. Morris, M. P. Hill, et al. "Coseismic deformation of the ground during large-slip strike-slip ruptures: Finite evolution of “mole tracks”." Geosphere 17, no. 4 (2021): 1170–92. http://dx.doi.org/10.1130/ges02336.1.

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Abstract To evaluate ground deformation resulting from large (~10 m) coseismic strike-slip displacements, we focus on deformation of the Kekerengu fault during the November 2016 Mw 7.8 Kaikōura earthquake in New Zealand. Combining post-earthquake field observations with analysis of high-resolution aerial photography and topographic models, we describe the structural geology and geomorphology of the rupture zone. During the earthquake, fissured pressure bulges (“mole tracks”) initiated at stepovers between synthetic Riedel (R) faults. As slip accumulated, near-surface “rafts” of cohesive clay-r
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McMechan, M. E. "Walker Creek fault zone, central Rocky Mountains, British Columbia-southern continuation of the Northern Rocky Mountain Trench fault zone." Canadian Journal of Earth Sciences 37, no. 9 (2000): 1259–73. http://dx.doi.org/10.1139/e00-038.

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Walker Creek fault zone (WCFZ), well exposed in the western Rocky Mountains of central British Columbia near 54°, comprises a 2 km wide zone of variably deformed Neoproterozoic and Cambrian strata in fault-bounded slivers and lozenges. Extensional shear bands, subhorizontal extension lineations, slickensides, mesoscopic shear bands, and other minor structures developed within and immediately adjacent to the fault zone consistently indicate right-lateral displacement. Offset stratigraphic changes in correlative Neoproterozoic strata indicate at least 60 km of right-lateral displacement across t
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Snyder, David B., Brian J. Roberts, and Steven P. Gordey. "Contrasting seismic characteristics of three major faults in northwestern Canada." Canadian Journal of Earth Sciences 42, no. 6 (2005): 1223–37. http://dx.doi.org/10.1139/e05-027.

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The Lithoprobe Slave – Northern Cordillera Lithospheric Evolution (SNORCLE) profiles crossed three major tectonic zones of the northwestern Canadian Shield and northern Canadian Cordillera that are diverse in age and in depth of penetration. The oldest (2630–2590 Ma), the Yellowknife River fault zone, formed as a strike-slip fault in a tensional strain regime. Reflector attenuation or truncations align vertically beneath the fault trace through much of the crust, implying a near-vertical fault plane. The youngest (60–10 Ma), the Tintina fault zone, produced cumulative dextral strike-slip displ
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Dissertations / Theses on the topic "Strike slip fault zone"

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Schmalzle, Gina Marie. "The Earthquake Cycle of Strike-Slip Faults." Scholarly Repository, 2008. http://scholarlyrepository.miami.edu/oa_dissertations/177.

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An earthquake is a mechanism of stress release along plate boundaries due to relative motion between the Earth's lithospheric blocks. The period in which stresses are accruing across the plate boundary is known as the interseismic portion of the earthquake cycle. This dissertation focuses on interseismic portion of the earthquake cycle to extract characteristics of fault, shear zone and rock properties. Global Positioning System (GPS) data are used to observe the pattern of deformation across two primarily strike-slip fault systems: the Carrizo Segment of the San Andreas Fault (SAF) and t
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Zhao, Peng. "Seismic velocity contrasts and temporal changes of strike-slip faults in central California." Diss., Georgia Institute of Technology, 2010. http://hdl.handle.net/1853/37242.

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The spatial patterns of bimaterial interfaces along the Parkfield section of the San Andreas Fault (SAF) and central section of the Calaveras Fault are systematically investigated with large data sets of near-fault waveforms. Different from the usage of direct P and S waves in traditional tomographic studies, a particular seismic phase named fault zone head wave (FZHW) is used to image the bimaterial fault interfaces. The results show clear variations of seismic velocities contrast both along-strike and along-depth directions in both regions, which is in general consistent with local geologica
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Hernandez, Moreno Catalina <1981&gt. "Understanding block rotation of strike-slip fault zones: Paleomagnetic and structural approach." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2015. http://amsdottorato.unibo.it/6829/.

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This thesis is focused on the paleomagnetic rotation pattern inside the deforming zone of strike-slip faults, and the kinematics and geodynamics describing it. The paleomagnetic investigation carried out along both the LOFZ and the fore-arc sliver (38º-42ºS, southern Chile) revealed an asymmetric rotation pattern. East of the LOFZ and adjacent to it, rotations are up to 170° clockwise (CW) and fade out ~10 km east of fault. West of the LOFZ at 42ºS (Chiloé Island) and around 39°S (Villarrica domain) systematic CCW rotations have been observed, while at 40°-41°S (Ranco-Osorno domain) and adja
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Canalda, Sabrina Michelle. "Magnitude of right-lateral offset on the southern Death Valley fault zone from miocene volcanic assemblages." To access this resource online via ProQuest Dissertations and Theses @ UTEP, 2009. http://0-proquest.umi.com.lib.utep.edu/login?COPT=REJTPTU0YmImSU5UPTAmVkVSPTI=&clientId=2515.

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Thornock, Steven Jesse. "Southward Continuation of the San Jacinto Fault Zone through and beneath the Extra and Elmore Ranch Left-Lateral Fault Arrays, Southern California." DigitalCommons@USU, 2013. https://digitalcommons.usu.edu/etd/1978.

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The Clark fault is one of the primary dextral faults in the San Jacinto fault zone system, southern California. Previous mapping of the Clark fault at its southern termination in the San Felipe Hills reveals it as a broad right lateral shear zone that ends north of the crossing, northeast-striking, left-lateral Extra fault. We investigate the relationship between the dextral Clark fault and the sinistral Extra fault to determine whether the Clark fault continues to the southeast. We present new structural, geophysical and geomorphic data that show that the Extra fault is a ~7 km wide, coordina
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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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Robeson, Kim R. "Three-Dimensional Structure of Small Strike-Slip Fault Zones in Granitic Rock: Implications for Fault-Growth Models." DigitalCommons@USU, 1998. https://digitalcommons.usu.edu/etd/5608.

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Three small strike-slip fault zones exposed in granitic rock in the central Sierra Nevada, California, provide field-based data to construct three-dimensional 11 representations of each fault zone in order to compare with the geometries predicted by existing fault-growth models. All three fault zones are nearly vertical, strike -N60°E, and have left-lateral slip. The fault zones range from 60 to 140 min length and 1 to 12 m wide. Each fault zone consists primarily of parallel to subparallel fracture and fault traces 2 to 56 m long and is separated 25 cm to 7 m by intact rock. One fault zone co
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Pachell, Matthew A. "Structural Analysis and a Kink Band Model for the Formation of the Gemini Fault Zone, an Exhumed Left-Lateral Strike Slip Fault Zone in the Central Sierra Nevada, California." DigitalCommons@USU, 2001. https://digitalcommons.usu.edu/etd/5244.

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The structure and regional tectonic setting of an exhumed, 9.3-km long, left-lateral strike-slip fault zone eludicates processes of growth, linkage, and termination for strike-slip fault zones in granitic rocks. The Gemini fault zone is composed of three steeply dipping, southwest-striking, noncoplanar segments that nucleated and grew along preexisting joints. The fault zone has a maximum slip of 131 m and is an example of a segmented, hard-linked fault zone in which geometrical complexities of the faults and compositional variations of protolith and host rock resulted in nonuniform slip orien
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Jaffey, Noah. "Cenozoic evolution of the strike-slip Ecemis fault zone and its implications for the mechanism of tectonic escape in Anatolia." Thesis, University of Edinburgh, 2001. http://hdl.handle.net/1842/12272.

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The mechanism by which crustal extrusion, or 'tectonic escape' functions remains poorly understood. Central Anatolia provides an example of extrusion where the kinematics of 'escape' - related strike-slip faults can be well-constrained. This study focuses on the Ecemis Fault Zone, one of the main strike-slip fault systems involved in the Cenozoic westward extrusion of Anatolia. This study concentrates on the structure, sedimentology, geomorphology and subsidence history of the EFZ, to constrain the timing and offset on this fault zone, and thereby build a more comprehensive model of extrusion
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Taylor, Tatia R. "ORIGIN AND STRUCTURE OF THE POVERTY HILLS, OWENS VALLEY FAULT ZONE, OWENS VALLEY, CALIFORNIA." Miami University / OhioLINK, 2002. http://rave.ohiolink.edu/etdc/view?acc_num=miami1021990715.

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Books on the topic "Strike slip fault zone"

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America, Geological Society of, ed. High geologic slip rates since early Pleistocene initiation of the San Jacinto and San Felipe fault zones in the San Andreas fault system, Southern California, USA. Geological Society of America, 2010.

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Sims, P. K. The Trans-Rocky Mountain fault system: A fundamental Precambrian strike-slip system. U.S. Dept. of the Interior, U.S. Geological Survey, 2009.

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Lee, Jeffrey, Daniel Stockli, Jeffrey Schroeder, et al., eds. Fault Slip Transfer in the Eastern California Shear Zone-Walker Lane Belt. Geological Society of America, 2006. http://dx.doi.org/10.1130/2006.fstite.pfg.

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W, Spengler Richard, United States. Dept. of Energy, and Geological Survey (U.S.), eds. The Sundance fault: A newly recognized shear zone at Yucca Mountain, Nevada. U.S. Dept. of the Interior, U.S. Geological Survey, 1994.

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B, Till Alison, ed. Exhumation associated with continental strike-slip fault systems. The Geological Society of America, 2007.

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Roeske, Sarah M., Alison B. Till, David A. Foster, and James C. Sample. Exhumation Associated with Continental Strike-Slip Fault Systems. Geological Society of America, 2007. http://dx.doi.org/10.1130/spe434.

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Special Paper 434: Exhumation Associated with Continental Strike-Slip Fault Systems. Geological Society of America, 2007. http://dx.doi.org/10.1130/978-0-8137-2434-8.

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Goldfinger, Chris. Active deformation of the Cascadia forearc: Implications for great earthquake potential in Oregon and Washington. 1994.

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1959-, Dolan James F., and Mann Paul 1956-, eds. Active strike-slip and collisional tectonics of the Northern Caribbean plate boundary zone. Geological Society of America, 1998.

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Dolan, James F., and Paul Mann. Active Strike-Slip and Collisional Tectonics of the Northern Caribbean Plate Boundary Zone. Geological Society of America, 1998. http://dx.doi.org/10.1130/spe326.

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Book chapters on the topic "Strike slip fault zone"

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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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de Joussineau, Ghislain, and Atilla Aydin. "Segmentation along Strike-Slip Faults Revisited." In Mechanics, Structure and Evolution of Fault Zones. Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0138-2_3.

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Aourari, Sahra, Djamel Machane, Hamid Haddoum, Saber Sedrati, Nadia Sidi Saîd, and Djillali Bouziane. "Neotectonic Analysis of an Alpine Strike Slip Fault Zone, Constantine Region, Eastern Algeria." In The Structural Geology Contribution to the Africa-Eurasia Geology: Basement and Reservoir Structure, Ore Mineralisation and Tectonic Modelling. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-030-01455-1_61.

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Finzi, 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. Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0138-2_2.

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Mann, Paul, and Mark B. Gordon. "Tectonic Uplift and Exhumation of Blueschist Belts Along Transpressional Strike-Slip Fault Zones." In Subduction Top to Bottom. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm096p0143.

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Goldfinger, Chris, LaVerne D. Kulm, Robert S. Yeats, et al. "Oblique Strike-Slip Faulting of the Cascadia Submarine Forearc: The Daisy Bank Fault Zone off Central Oregon." In Subduction Top to Bottom. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm096p0065.

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Swanson, Mark T. "Pseudotachylyte-bearing strike-slip faults in mylonitic host rocks, Fort Foster Brittle Zone, Kittery, Maine." In Earthquakes: Radiated Energy and the Physics of Faulting. American Geophysical Union, 2006. http://dx.doi.org/10.1029/170gm17.

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Dubey, Ashok Kumar. "Strike-Slip Fault." In Understanding an Orogenic Belt. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-05588-6_6.

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Kilgore, Brian D., Art McGarr, Nicholas M. Beeler, and David A. Lockner. "Earthquake Source Properties From Instrumented Laboratory Stick-Slip." In Fault Zone Dynamic Processes. John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch8.

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Karasaki, Kenzi, Celia T. Onishi, and Junichi Goto. "Permeability Structure of a Strike-Slip Fault." In Dynamics of Fluids and Transport in Complex Fractured-Porous Systems. John Wiley & Sons, Inc, 2015. http://dx.doi.org/10.1002/9781118877517.ch3.

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Conference papers on the topic "Strike slip fault zone"

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Wang, Wei, Kui Wu, Lin Kang, Xiaobo Huang, and Jian Yao. "Buried Strike-Slip Fault Identification Technique Based on a 3D Stress Body Attribute Considering Formation Deformation and Lithologic Variation." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21442-ms.

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Abstract The identification and interpretation of buried strike-slip faults are of great significance int the search for structural traps in oil and gas exploration. However, it is difficult to identify and interpret buried strike-slip faults from seismic profiles and variance slicing, because they may be clear at depth but vague in the shallow. This study proposes a 3D stress body attribute taking into consideration formation deformation and lithologic variation to identify buried strike-slip faults. Taking into account thin plate theory and the generalized Hooke's law, a relationship between
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Scharman, Mitchell R. "DEXTRAL STRIKE-SLIP OVERPRINT ON THE BYLLESBY-FALLS FAULT ZONE, IRON MOUNTAINS, SOUTHWESTERN VIRGINIA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-279919.

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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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Sullivan, Walter A. "RHEOLOGIC EVOLUTION OF A CRUSTAL-SCALE STRIKE-SLIP FAULT ZONE: A CASE STUDY OF THE KELLYLAND FAULT ZONE IN EASTERN MAINE." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328268.

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Ikhwanudin, Fahmi, and Chalid Idham Abdullah. "Indication Strike Slip Movement A Part of Sorong Fault Zone in Yapen Island, Papua, Indonesia." In Annual International Conference on Geological & Earth Sciences. Global Science & Technology Forum (GSTF), 2014. http://dx.doi.org/10.5176/2251-3353_geos14.24.

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Clemenzi, L., F. Balsamo, F. Storti, et al. "Structural Architecture and Paleofluid Evolution of Strike-slip and Normal Fault Zones, Jabal Qusaybah Anticline, Oman." In Fourth International Conference on Fault and Top Seals. EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201414091.

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Langenheim, Victoria, Robert McLaughlin, and Benjamin L. Melosh. "GEOLOGIC AND GEOPHYSICAL CHARACTERIZATION OF THE BARTLETT SPRINGS FAULT ZONE (CALIFORNIA): IMPLICATIONS FOR FAULT BEHAVIOR AND EVOLUTION OF A MAJOR STRIKE-SLIP FAULT." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-354450.

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Zhang, A. D., B. J. C. Li, C. W. J. Zhao, and D. Z. H. Wu. "Application of ground penetrating radar to active faults along Yushu strike-slip faults zone, Qinghai, China." In 15th International Conference on Ground-Penetrating Radar (GPR) 2014. IEEE, 2014. http://dx.doi.org/10.1109/icgpr.2014.6970436.

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Lescalleet, Nolan Thomas, Matthew R. F. Manon, and Kristin Morell. "THE SAN JUAN FAULT, AN E-W TRENDING LEFT-LATERAL STRIKE SLIP FAULT ZONE INFERRED FROM ANALYSIS OF KINEMATIC INDICATORS; VANCOUVER ISLAND, CANADA." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-291472.

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Zhang, Zhiqiang, Donghong Zhou, Liqun Jiang, Wenxu Peng, and Deying Wang. "Analysis of strike-slip fault zone using multiazimuth 3D seismic data: A case study on the western Offshore Bohai Bay." In SEG Technical Program Expanded Abstracts 2012. Society of Exploration Geophysicists, 2012. http://dx.doi.org/10.1190/segam2012-0342.1.

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Reports on the topic "Strike slip fault zone"

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Davis, George. Structural Geologic Maps of Conjugate Normal-Fault and Strike-Slip Deformation Band Shear Zones in Navajo Sandstone. Geological Society of America, 2013. http://dx.doi.org/10.1130/2013.dmch015.1.

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Foxall, William. Heterogeneous slip and rupture models of the San Andreas fault zone based upon three-dimensional earthquake tomography. Office of Scientific and Technical Information (OSTI), 1992. http://dx.doi.org/10.2172/10163876.

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Lewis, P. D. Dextral Strike - Slip Faulting and Associated Extension Along the southern Portion of the Louscoone Inlet Fault System, southern Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132536.

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Cruikshank, K. M., A. M. Johnson, R. W. Fleming, and R. L. Jones. Winnetka deformation zone: Surface expression of coactive slip on a blind fault during the Northridge earthquake sequence, California. Evidence that coactive faulting occurred in the Canoga Park, Winnetka, and Northridge areas during the 17 January 1994, Northridge, California earthquake. Office of Scientific and Technical Information (OSTI), 1996. http://dx.doi.org/10.2172/677055.

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High-resolution multichannel seismic-reflection profiles across the Helena Banks strike-slip fault zone offshore of the Charleston, South Carolina, earthquake area. US Geological Survey, 1988. http://dx.doi.org/10.3133/mf2056.

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