Relevant bibliographies by topics / Fault depth

Contents

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

Academic literature on the topic 'Fault depth'

Author: Grafiati
Published: 3 June 2025
Last updated: 31 July 2025

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Journal articles on the topic "Fault depth"

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Chávez‐Pérez, Sergio, John N. Louie, and Sathish K. Pullammanappallil. "Seismic depth imaging of normal faulting in the southern Death Valley Basin." GEOPHYSICS 63, no. 1 (1998): 223–30. http://dx.doi.org/10.1190/1.1444316.

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Motivated by the need to image faults to test Cenozoic extension models for the Death Valley region of the western basin and range province, an area of strong lateral velocity variations, we examine the geometry of normal faulting in southern Death Valley by seismic depth imaging. We analyze COCORP Death Valley Line 9 to attain an enhanced image of shallow fault structure to 2.5 km depth. Previous work used standard seismic processing to infer normal faults from bed truncations, displacement of horizontal reflectors, and diffractions. We obtain a detailed velocity model by nonlinear optimizati
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Oglesby, David D. "What Can Surface-Slip Distributions Tell Us about Fault Connectivity at Depth?" Bulletin of the Seismological Society of America 110, no. 3 (2020): 1025–36. http://dx.doi.org/10.1785/0120190245.

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ABSTRACT Fault systems with stepovers and gaps along strike are ubiquitous in nature, and many modern earthquakes (e.g., 1992 Landers, 1999 Hector Mine, 2016 Kaikōura, and 2019 Ridgecrest) have shown that ruptures can readily propagate across some disconnections, while being halted by others. It is quite possible, however, that many faults that appear discontinuous at the surface are in fact connected at depth, facilitating throughgoing rupture, and potentially increasing earthquake size. The present work explores whether the mapped surface slip in an earthquake is indicative of the connectivi
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Ibrahim, Elkhedr, Mohamed Arfaoui, Saad Mogren, Saleh Qaysi, Aref Lashin, and Hussain Alfaifi. "Disposition of magmatic eruptions and fault distribution in northwestern Saudi Arabia using pseudo-depth slice magnetic anomaly." Journal of Geophysics and Engineering 18, no. 4 (2021): 463–81. http://dx.doi.org/10.1093/jge/gxab028.

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Abstract This study presents the disposition of magmatic eruptions with a fault distribution in northwestern Saudi Arabia, where intensive magma invades the lithosphere. Structural and magmatic features are traced at successive depths through high-resolution magnetic anomaly pseudo-depth slices. The total horizontal gradient technique is applied to pseudo-depth slice magnetic anomalies to enhance the linear trends of faults and related magmatic activity. A comprehensive cross-section constructed from the projection of gradient horizontal maxima relative to pseudo-slices allows the visualizatio
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Catchings, R. D., M. R. Goldman, W. H. K. Lee, M. J. Rymer, and D. J. Ponti. "Faulting apparently related to the 1994 Northridge, California, earthquake and possible co-seismic origin of surface cracks in Potrero Canyon, Los Angeles County, California." Bulletin of the Seismological Society of America 88, no. 6 (1998): 1379–91. http://dx.doi.org/10.1785/bssa0880061379.

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Abstract Apparent southward-dipping, reverse-fault zones are imaged to depths of about 1.5 km beneath Potrero Canyon, Los Angeles County, California. Based on their orientation and projection to the surface, we suggest that the imaged fault zones are extensions of the Oak Ridge fault. Geologic mapping by others and correlations with seismicity studies suggest that the Oak Ridge fault is the causative fault of the 17 January 1994 Northridge earthquake (Northridge fault). Our seismically imaged faults may be among several faults that collectively comprise the Northridge thrust fault system. Unus
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Ghose, Ritu, Patricia Persaud, and Robert W. Clayton. "Basin Structure for Earthquake Ground Motion Estimates in Urban Los Angeles Mapped with Nodal Receiver Functions." Geosciences 13, no. 11 (2023): 320. http://dx.doi.org/10.3390/geosciences13110320.

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We constrained sedimentary basin structure using a nodal seismic array consisting of ten dense lines that overlie multiple basins in the northern Los Angeles area. The dense array consists of 758 seismic nodes, spaced ~250–300 m apart along linear transects, that recorded ground motions for 30–35 days. We applied the receiver function (RF) technique to 16 teleseismic events to investigate basin structure. Primary basin-converted phases were identified in the RFs. A shear wave velocity model produced in a separate study using the same dataset was incorporated to convert the basin time arrivals
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Barbosa, Valeria C., Paulo T. Menezes, and João B. Silva. "Gravity data as a tool for detecting faults: In-depth enhancement of subtle Almada’s basement faults, Brazil." GEOPHYSICS 72, no. 3 (2007): B59—B68. http://dx.doi.org/10.1190/1.2713226.

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We demonstrate the potential of gravity data to detect and to locate in-depth subtle normal faults in the basement relief of a sedimentary basin. This demonstration is accomplished by inverting the gravity data with the constraint that the estimated basement relief presents local abrupt faults and is smooth elsewhere. We inverted the gravity data from the onshore Almada Basin in northeastern Brazil, and we mapped several normal faults whose locations and plane geometries were already known from seismic imaging. The inversion method delineated well both the discontinuities with small or large s
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Asensio, Eduardo Maximiliano, Ken King Man Siu, Juan Carlos Astrada, Federico Martín Serra, and Cristian Hernán De Angelo. "Comprehensive Analysis and Reconstruction of Sensor Faults in Interleaved Buck Converters Using Sliding Mode Observers." Electronics 13, no. 21 (2024): 4202. http://dx.doi.org/10.3390/electronics13214202.

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This paper presents a fault signal reconstruction method for current sensors in an interleaved buck DC–DC converter, utilizing a sliding mode observer (SMO). A filter bank is used to design the observer within an extended-order system, effectively treating sensor faults as actuator faults, which enables precise estimation of the fault signal. Thus, the proposed approach allows for the identification of the faulty sensor and supports the implementation of fault-tolerant strategies. The paper provides an in-depth analysis of current sensor faults, verifies their impact on current balancing contr
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Birdus, Sergey, and Alexey Artyomov. "Removing fault shadow distortions from seismic images using depth-velocity modelling and pre-stack depth migration." APPEA Journal 52, no. 2 (2012): 700. http://dx.doi.org/10.1071/aj11114.

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In many areas, fault shadows manifest a serious challenge to seismic imaging. The major part of this problem is caused by different types of velocity variations caused by faults. Pre-stack depth migration with sufficiently accurate velocity model successfully resolves this problem and the high resolution tomographic depth-velocity modelling is the most important component of the solution. During depth processing on a number of real 3D seismic datasets with fault shadows from Australia and other regions, the following were noticed: The appearance of the image distortions below the faults and th
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Doser, Diane I. "Source parameters of Montana earthquakes (1925-1964) and tectonic deformation in the northern Intermountain Seismic Belt." Bulletin of the Seismological Society of America 79, no. 1 (1989): 31–50. http://dx.doi.org/10.1785/bssa0790010031.

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Abstract Waveform modeling and first motion analysis are used to determine the source parameters of six 5.8 ≦ M ≦ 6.8 earthquakes that occurred between 1925 and 1964 within the northern Intermountain Seismic Belt of Montana. Results of this study suggest that the 1925 Clarkston earthquake occurred along an oblique normal fault with a trend similar to the southern end of the Clarkston Valley fault. The two largest earthquakes of the 1935 Helena sequence occurred along right-lateral strike-slip faults with trends similar to the Bald Butte and Helena Valley faults. The 1947 Virginia City earthqua
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Ahmadi, O., C. Juhlin, M. Ask, and B. Lund. "Revealing the deeper structure of the end-glacial Pärvie fault system in northern Sweden by seismic reflection profiling." Solid Earth 6, no. 2 (2015): 621–32. http://dx.doi.org/10.5194/se-6-621-2015.

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Abstract. A new seismic reflection survey for imaging deeper levels of the end-glacial Pärvie fault system in northern Sweden was acquired in June 2014. The Pärvie fault system hosts the largest fault scarp so far documented in northern Scandinavia, both in terms of its length and calculated magnitude of the earthquake that generated it. Present-day microearthquakes occur along the length of the fault scarp on the eastern side of the scarp, in general agreement with an east-dipping main fault. In the central section of the fault system, where there is a number of subsidiary faults east of the
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Dissertations / Theses on the topic "Fault depth"

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Keighley, Bradbury Kelly. "Rock Properties and Structure Within the San Andreas Fault Observatory at Depth (SAFOD) Borehold, Northwest of Parkfield, California: In Situ Observations of Rock Deformation Processes and Fluid-Rock Interactions of the San Andreas Fault Zone at ~ 3 km Depth." DigitalCommons@USU, 2012. https://digitalcommons.usu.edu/etd/1410.

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This project examines the composition, structure, and geophysical properties of rocks sampled within the San Andreas Fault Observatory at Depth (SAFOD) borehole drilling experiment near Parkfield, California. Cuttings, sidewall cores, spot-core, and whole-rock core are examined from the meso- to micro-scale to characterize the nearfault environment at shallow crustal levels (0-4 km) along the central segment of the San Andreas fault. The central segment deforms by contiuous aseismic creep and microseismicity. An integrated approach utilizing core-logging, detailed structural core mapping, petr
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Otsubo, Makoto. "Depth-dependent state of stress revealed by fault-slip analysis in the Niigata fold belt, Japan." 京都大学 (Kyoto University), 2006. http://hdl.handle.net/2433/144200.

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Kyoto University (京都大学)<br>0048<br>新制・課程博士<br>博士(理学)<br>甲第12117号<br>理博第3011号<br>新制||理||1449(附属図書館)<br>23953<br>UT51-2006-J112<br>京都大学大学院理学研究科地球惑星科学専攻<br>(主査)助教授 山路 敦, 教授 増田 富士雄, 教授 小畑 正明<br>学位規則第4条第1項該当
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Broda, Cynthia Marie. "Ontology and Knowledge Base of Brittle Deformation Microstructures for the San Andreas Fault Observatory at Depth (SAFOD) Core Samples." Digital Archive @ GSU, 2010. http://digitalarchive.gsu.edu/geosciences_theses/26.

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The quest to answer fundamental questions and solve complex problems is a principal tenet of Earth science. The pursuit of scientific knowledge has generated profuse research, resulting in a plethora of information-rich resources. This phenomenon offers great potential for scientific discovery. However, a deficiency in information connectivity and processing standards has become evident. This deficiency has resulted in a demand for tools to facilitate and process this upsurge in information. This ontology project is an answer to the demand for information processing tools. The primary purpose
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Draper, Sarah D. "The Geologic History of Subsurface Arkosic Sedimentary Rocks in the San Andreas Fault Observatory at Depth (SAFOD) Borehole, Central California." DigitalCommons@USU, 2007. https://digitalcommons.usu.edu/etd/6021.

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The aim of the San Andreas Fault Observatory at Depth (SAFOD) project, a component of the NSF Earthscope Initiative, is to directly observe active fault processes at seismogenic depths through the drilling of a 3 km deep (true vertical depth) inclined borehole across San Andreas fault. Preliminary subsurface models based on surface mapping and geophysical data predicted different lithologies than were actually encountered. At 1920 meters measured depth (mmd), a sequence of well-indurated, interbedded arkosic conglomerates, sandstones, and siltstones was encountered. We present a detailed litho
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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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Hayman, Nicholas W. "Structure and petrology of gouge and breccia bearing shallow crustal shear zones of detachment faults in Death Valley, California /." Thesis, Connect to this title online; UW restricted, 2005. http://hdl.handle.net/1773/6699.

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Lawther, Susan E. M. "The effects of fluid flow through faults in granite gneiss exhumed from seismogenic depths." Thesis, University of Glasgow, 2012. http://theses.gla.ac.uk/3374/.

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Fault zones are ubiquitous structures throughout the Earth’s crust and as a fault evolves it can significantly influence the rheological and hydrological properties of the crust. Fluid flow through fault zones is typically associated with fault-fluid-rock interactions and these interactions can affect the mineralogy, strength and evolution of a fault zone. In this study, field mapping is combined with petro-physical and stable isotopic analyses of the fault rock to evaluate the fault-fluid-rock interactions that occur within different fault zones, and the effects of these reactions on fault zo
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Miller, Martin Gregg. "Structural and kinematic evolution of the Badwater Turtleback, Death Valley, California /." Thesis, Connect to this title online; UW restricted, 1992. http://hdl.handle.net/1773/6716.

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Guerrero, Francisco Jesus. "Death Valley reconstruction new piercingpoints in the Panamint Mountains and Resting Springs Range /." To access this resource online via ProQuest Dissertations and Theses @ UTEP, 2008. http://0-proquest.umi.com.lib.utep.edu/login?COPT=REJTPTU0YmImSU5UPTAmVkVSPTI=&clientId=2515.

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Wamalwa, Antony Munika. "Geophysical investigations of ground water flow associated with the Saratoga Warm Springs and the Tecopa Hot Springs near Death Valley Callifornia." To access this resource online via ProQuest Dissertations and Theses @ UTEP, 2008. http://0-proquest.umi.com.lib.utep.edu/login?COPT=REJTPTU0YmImSU5UPTAmVkVSPTI=&clientId=2515.

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Books on the topic "Fault depth"

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Canada, Atomic Energy of. Structural analysis of the thrust fault at a depth of 271 to 275 m in the underground research laboratory shaft. s.n, 1988.

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Flynn, Jessie. It's not your fault. J. Flynn, 1994.

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Eisler, Barry. Fault Line. Random House Publishing Group, 2009.

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Eisler, Barry. Fault line: [a novel]. Books on Tape, 2009.

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Eisler, Barry. Fault line: A novel. Random House Large Print, 2009.

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Faunt, Claudia C. Effect of faulting on ground-water movement in the Death Valley Region, Nevada and California. U.S. Dept. of the Interior, U.S. Geological Survey, 1997.

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Green, John. The fault in our stars. Thorndike Press, 2012.

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Frances, Stephen. The Fault in Our Stars. Penguin Books, 2014.

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Buckman, Rob. Que faut-il dire? Québécor, 1989.

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Brogan, George E. Late Quaternary faulting along the Death Valley-Furnace Creek fault system, California and Nevada. [s.n.], 1992.

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Book chapters on the topic "Fault depth"

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Brantut, Nicolas, and John D. Platt. "Dynamic Weakening and the Depth Dependence of Earthquake Faulting." In Fault Zone Dynamic Processes. John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch9.

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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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Bauer, Waldemar, Adrian Dudek, and Jerzy Baranowski. "Comparison of Data Depth Calculation Method for Fault Detection in Electric Signal." In Advanced, Contemporary Control. Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-35173-0_5.

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Bilek, Susan L., and Thorne Lay. "Comparison of Depth Dependent Fault Zone Properties in the Japan Trench and Middle America Trench." In Seismogenic and Tsunamigenic Processes in Shallow Subduction Zones. Birkhäuser Basel, 1999. http://dx.doi.org/10.1007/978-3-0348-8679-6_3.

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Rasouli, Habib, and Behzad Fatahi. "Effect of Burial Depth on Pipeline-Fault Rupture Interaction Mechanism and Mitigation Technique Using Geofoam Blocks." In Challenges and Innovations in Geomechanics. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-64518-2_115.

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Annas, George J. "No Fault Death." In Judging Medicine. Humana Press, 1988. http://dx.doi.org/10.1007/978-1-4612-4592-6_40.

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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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Yang, Liu, Zedong Du, Zhiren Feng, and Bo Jin. "Spatial Characteristics of Basic Storage Media of Reservoir-Induced Earthquakes in the Lower Reaches of Jinsha River—A Case Study in Baitan-Zhilixincun." In Lecture Notes in Civil Engineering. Springer Nature Singapore, 2024. http://dx.doi.org/10.1007/978-981-97-7251-3_4.

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AbstractReservoir-induced earthquakes have the characteristics of shallow focal depth, small magnitude, high frequency and density in the Baitan-Zhilixincun section of the lower reaches of the Jinsha River. The rock mass of the shallow strata is mostly carbonate rock, which is widely distributed. The shallow metamorphic rocks are mainly distributed at the depth of 10 km. In the concentrated area of reservoir-induced earthquakes, the number of secondary faults is relatively large, and they are mainly reverse faults. The stress and strain patterns of the shallow cracks are mainly unloading crack
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Shevtchenko, V. "On the Depth of Decision Trees for Diagnosing of Nonelementary Faults in Circuits." In Rough Sets and Current Trends in Computing. Springer Berlin Heidelberg, 1998. http://dx.doi.org/10.1007/3-540-69115-4_71.

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Fagin, Stuart. "11. Case History 1 Solving the Fault Shadow Problem." In Model-Based Depth Imaging. Society of Exploration Geophysicists, 1998. http://dx.doi.org/10.1190/1.9781560802013.ch11.

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Conference papers on the topic "Fault depth"

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Kim, Yong Chae, Seungyun Lee, Sang Kyung Lee, et al. "Inter-class Metric Learning based Depth-wise Convolutional Neural Network for Gear Fault Diagnosis." In 2024 IEEE International Conference on Prognostics and Health Management (ICPHM). IEEE, 2024. http://dx.doi.org/10.1109/icphm61352.2024.10626900.

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Zhao, Hongwei, Vianney Lapôtre, and Guy Gogniat. "Communication Architecture Under Siege: An In-depth Analysis of Fault Attack Vulnerabilities and Countermeasures." In 2024 IEEE International Conference on Cyber Security and Resilience (CSR). IEEE, 2024. http://dx.doi.org/10.1109/csr61664.2024.10679464.

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Zeng, Yun, and Ming Deng. "Multi-Objective Two-Stage Fault Recovery Method for Distribution Network Based on Heterogeneous Feature Depth Extraction." In 2024 Boao New Power System International Forum - Power System and New Energy Technology Innovation Forum (NPSIF). IEEE, 2024. https://doi.org/10.1109/npsif64134.2024.10883582.

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Sethi, Madhav, Kanwarpartap Singh Gill, Rahul Chauhan, and Hemant Singh Pokhariya. "Unlocking the Potential of AdaBoost through In-Depth Study of its Efficiency in Electrical Fault Detection." In 2024 International Conference on Control, Computing, Communication and Materials (ICCCCM). IEEE, 2024. https://doi.org/10.1109/iccccm61016.2024.11039917.

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Kim, Keonil, Kyunghoon Shin, and Ghil-Geun Oh. "Enhanced Dynamic Laser Stimulation Method for Fault Isolation." In ISTFA 2024. ASM International, 2024. http://dx.doi.org/10.31399/asm.cp.istfa2024p0039.

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Abstract Optical Fault Isolation (OFI) techniques have been still very effective method for semiconductor failure analysis such as silicon (Si) debugging and defect localization. Dynamic Laser Stimulation (DLS) is one of the most powerful application not only for marginal failure but also to isolate the potential design weak point at the early phase of product development. However, as circuit density of recent advanced system on chip (SoC) extremely increases with process scaling down, vector depth of products are also dramatically increased. This presents a challenging aspect for failure anal
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Aretakis, N., I. Roumeliotis, and K. Mathioudakis. "Performance Model “Zooming” for In-Depth Component Fault Diagnosis." In ASME Turbo Expo 2010: Power for Land, Sea, and Air. ASMEDC, 2010. http://dx.doi.org/10.1115/gt2010-23262.

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A method giving the possibility for a more detailed gas path component fault diagnosis, by exploiting the “zooming” feature of current performance modelling techniques, is presented. A diagnostic engine performance model is the main tool that points to the faulty engine component. A diagnostic component model is then used to identify the fault. The method is demonstrated on the case of compressor faults. A 1-D model based on the “stage stacking” approach is used to “zoom” into the compressors, supporting a 0-D engine model. A first level diagnosis determines the deviation of overall compressor
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Zhang, Jieyu, and Mirko van der Baan. "Depth-dependent fault slip potential." In SEG Technical Program Expanded Abstracts 2019. Society of Exploration Geophysicists, 2019. http://dx.doi.org/10.1190/segam2019-3214231.1.

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Khaireddine, Besma, Aleksandr Zakharchenko, and Ali Mili. "Fault Density, Fault Depth and Fault Multiplicity: The Reward of Discernment." In 2019 IEEE 19th International Conference on Software Quality, Reliability and Security Companion (QRS-C). IEEE, 2019. http://dx.doi.org/10.1109/qrs-c.2019.00110.

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Khaireddine, Besma, Matias Martinez, and Ali Mili. "Program Repair at Arbitrary Fault Depth." In 2019 12th IEEE Conference on Software Testing, Validation and Verification (ICST). IEEE, 2019. http://dx.doi.org/10.1109/icst.2019.00056.

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Schuller, Volker, Andras Zamolyi, Eirik Stueland, István Dunkl, Michael Kettermann, and Zsolt Schleder. "Fault Rock Property Prediction On Jurassic Clastics Of The Barents Sea/Norway." In SPE Annual Technical Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/206290-ms.

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Abstract We analysed the fault rocks of a compartmentalized field in the Barents Sea, in an area with several tectonic elements, which formed at different tectonic events. Standard Fault Seal Analysis (FSA) was conducted to predict the shale content of the fault rock (SGR). A static cellular model based on well data, seismic data and geological concepts served as input. The fault rock calibration workflow required various data acquired by different methods. We analysed the Mid-Triassic to Upper Jurassic clastic deposits to reconstruct the tectonic history. Apatite fission track and (U-Th)/He t
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Reports on the topic "Fault depth"

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Boots, Byron, Jacob Sacks, Kevin Choi, et al. Downhole Sensing and Event-Driven Sensor Fusion for Depth-of-Cut Based Autonomous Fault Response and Drilling Optimization. Office of Scientific and Technical Information (OSTI), 2023. http://dx.doi.org/10.2172/2430188.

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Paul, C., and J. F. Cassidy. Seismic hazard investigations at select DND facilities in Southwestern British Columbia: subduction, in-slab, and crustal scenarios. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/331199.

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Southwest British Columbia has some of the highest seismic hazard in Canada and is home to facilities owned by the Department of National Defence which support operations on the west coast of Canada. The potential impact of seismic hazards on these government facilities are investigated here. The hazard is from three primary sources: subduction interface, crustal and in-slab earthquakes. NRCan, in consultation with DRDC have produced representative earthquake scenarios for each of these sources. The subduction scenario we constructed was an M8.9 earthquake extending along the entire Cascadia S
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Hayward, N., and S. Paradis. Geophysical reassessment of the role of ancient lineaments on the development of the western margin of Laurentia and its sediment-hosted Zn-Pb deposits, Yukon and Northwest Territories. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330038.

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The role of crustal lineaments in the development of the western margin of Laurentia, Selwyn basin and associated sediment-hosted Zn-Pb deposits (clastic-dominated, Mississippi-Valley-type) in Yukon and NWT, are reassessed through a new 3-D inversion strategy applied to new compilations of gravity and magnetic data. Regionally continuous, broadly NE-trending crustal lineaments including the Liard line, Fort Norman structure, and Leith Ridge fault, were interpreted as having had long-standing influence on craton, margin, and sedimentary basin development. However, multiple tectonic overprints i
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Douglas, K., J. V. Barrie, T. Dill, T. Fralic, and N. Koshure. 2021004PGC cruise report: mapping Salish Sea marine geohazards, British Columbia. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329621.

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The Geological Survey of Canada (GSC) undertook marine fieldwork onboard the Canadian Coast Guard Ship (CCGS) Vector to locate and map potential geohazards and geological features in the Salish Sea in the interest of public safety from August 11-18, 2021. This work was conducted under the Natural Resources Canada Marine Geoscience for Marine Spatial Planning (MGMSP) and the Public Safety Geoscience Programs. The GSC had observed multiple potential faults in existing data near Central Haro Strait, Stuart Channel, South of Hornby Island and near Cape Lazo through existing CHIRP and multibeam bat
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Abrahamson, Norman, Nicolas Kuehn, Zeynep Gulerce, et al. Update of the BC Hydro Subduction Ground-Motion Model using the NGA- Subduction Dataset. Pacific Earthquake Engineering Research Center, University of California, Berkeley, CA, 2018. http://dx.doi.org/10.55461/oycd7434.

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An update to the BCHydro ground-motion model for subduction earthquakes has been developed using the 2018 PEER NGA-SUB dataset. The selected subset includes over 70,000 recordings from 1880 earthquakes. The update modifies the BCHydro model to include regional terms for the VS30 scaling, large distance (linear R) scaling, and constant terms, which is consistent with the regionalization approach used in the NGA-W2 ground-motion models. A total of six regions were considered: Cascadia, Central America, Japan, New Zealand, South America, and Taiwan. Region- independent terms are used for the smal
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Harris, L. B., P. Adiban, and E. Gloaguen. The role of enigmatic deep crustal and upper mantle structures on Au and magmatic Ni-Cu-PGE-Cr mineralization in the Superior Province. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328984.

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Aeromagnetic and ground gravity data for the Canadian Superior Province, filtered to extract long wavelength components and converted to pseudo-gravity, highlight deep, N-S trending regional-scale, rectilinear faults and margins to discrete, competent mafic or felsic granulite blocks (i.e. at high angles to most regional mapped structures and sub-province boundaries) with little to no surface expression that are spatially associated with lode ('orogenic') Au and Ni-Cu-PGE-Cr occurrences. Statistical and machine learning analysis of the Red Lake-Stormy Lake region in the W Superior Province con
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Onuoha, Chukwuma Candidus, and Shamus McDonnell. PR-388-143604-R01 Identifying Coating Faults and Severity Through Electrolyte Resistivity Measurement. Pipeline Research Council International, Inc. (PRCI), 2018. http://dx.doi.org/10.55274/r0011481.

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Soil resistivity is one of the most important variables that is used to ascertain the corrosivity of an electrolyte around a pipe. This is crucial information that enhances the classification, prioritization and selection of locations prone to external corrosion during External Corrosion Direct Assessment (ECDA) or pipeline integrity assessment when combined with results from cathodic protection and coating surveys. The Wenner Four-Pin method is commonly used in the industry for soil resistivity measurements. It entails perpendicular measurements with four equidistant pins away from the pipe t
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Arcone, Steven, James Lever, Laura Ray, Benjamin Walker, Gordon Hamilton, and Lynn Kaluzienski. Ground-penetrating radar profiles of the McMurdo shear zone, Antarctica, acquired with an unmanned rover : interpretation of crevasses, fractures, and folds within firn and marine ice. Engineer Research and Development Center (U.S.), 2021. http://dx.doi.org/10.21079/11681/42620.

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The crevassed firn of the McMurdo shear zone (SZ) within the Ross Ice Shelf may also contain crevasses deep within its meteoric and marine ice, but the surface crevassing prevents ordinary vehicle access to investigate its structure geophysically. We used a lightweight robotic vehicle to tow 200- and 40 MHz ground-penetrating radar antennas simultaneously along 10 parallel transects over a 28 km² grid spanning the SZ width. Transects were generally orthogonal to the ice flow. Total firn and meteoric ice thickness was approximately 160 m. Firn crevasses profiled at 400 MHz were up to 16 m wide,
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Farahbod, A. M., and J. F. Cassidy. An overview of seismic attenuation in the Eastern Canadian Arctic and the Hudson Bay Complex, Manitoba, Newfoundland and Labrador, Nunavut, Ontario, and Quebec. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330396.

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In this study we investigated coda-wave attenuation (QC) from the eastern Canadian Arctic in Nunavut and the Hudson Bay complex including portions of northern Manitoba, Ontario, Quebec and Labrador. We used earthquake recordings from 15 broadband and 3 short period seismograph stations of the Canadian National Seismic Network (CNSN) and 29 broadband stations of the POLARIS network across the region. Our dataset is comprised of 637 earthquakes recorded between 1985 and 2021 with magnitudes ranging from 1.3 to 6.1, depths from 0 to 20 km and epicentral distances of 5 to 100 km. This gives a tota
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Reheis, M. C., and J. S. Noller. Aerial photographic interpretation of lineaments and faults in late cenozoic deposits in the Eastern part of the Benton Range 1:100,000 quadrangle and the Goldfield, Last Chance Range, Beatty, and Death Valley Junction 1:100,000 quadrangles, Nevada and California. Office of Scientific and Technical Information (OSTI), 1991. http://dx.doi.org/10.2172/138195.

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