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Relevant bibliographies by topics / Physical properties of fault zones

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Academic literature on the topic 'Physical properties of fault zones'

Author: Grafiati

Published: 25 May 2024

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Journal articles on the topic "Physical properties of fault zones"

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Verberne, Berend A., Oliver Plümper, and Christopher J. Spiers. "Nanocrystalline Principal Slip Zones and Their Role in Controlling Crustal Fault Rheology." Minerals 9, no. 6 (2019): 328. http://dx.doi.org/10.3390/min9060328.

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Principal slip zones (PSZs) are narrow (<10 cm) bands of localized shear deformation that occur in the cores of upper-crustal fault zones where they accommodate the bulk of fault displacement. Natural and experimentally-formed PSZs consistently show the presence of nanocrystallites in the <100 nm size range. Despite the presumed importance of such nanocrystalline (NC) fault rock in controlling fault mechanical behavior, their prevalence and potential role in controlling natural earthquake cycles remains insufficiently investigated. In this contribution, we summarize the physical properti

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Gibson, Richard G. "Physical character and fluid-flow properties of sandstone-derived fault zones." Geological Society, London, Special Publications 127, no. 1 (1998): 83–97. http://dx.doi.org/10.1144/gsl.sp.1998.127.01.07.

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Guillou-Frottier, Laurent, Hugo Duwiquet, Gaëtan Launay, Audrey Taillefer, Vincent Roche, and Gaétan Link. "On the morphology and amplitude of 2D and 3D thermal anomalies induced by buoyancy-driven flow within and around fault zones." Solid Earth 11, no. 4 (2020): 1571–95. http://dx.doi.org/10.5194/se-11-1571-2020.

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Abstract. In the first kilometers of the subsurface, temperature anomalies due to heat conduction processes rarely exceed 20–30 ∘C. When fault zones are sufficiently permeable, fluid flow may lead to much larger thermal anomalies, as evidenced by the emergence of thermal springs or by fault-related geothermal reservoirs. Hydrothermal convection triggered by buoyancy effects creates thermal anomalies whose morphology and amplitude are not well known, especially when depth- and time-dependent permeability is considered. Exploitation of shallow thermal anomalies for heat and power production part

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Zoback, M., S. Hickman, and W. Ellsworth. "Scientific Drilling Into the San Andreas Fault Zone – An Overview of SAFOD's First Five Years." Scientific Drilling 11 (March 1, 2011): 14–28. http://dx.doi.org/10.5194/sd-11-14-2011.

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The San Andreas Fault Observatory at Depth (SAFOD) was drilled to study the physical and chemical processes controlling faulting and earthquake generation along an active, plate-bounding fault at depth. SAFOD is located near Parkfield, California and penetrates a section of the fault that is moving due to a combination of repeating microearthquakes and fault creep. Geophysical logs define the San Andreas Fault Zone to be relatively broad (~200 m), containing several discrete zones only 2&ndash;3 m wide that exhibit very low P- and S-wave velocities and low resistivity. Two of these zones h

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Pampillón, Pedro, David Santillán, Juan Carlos Mosquera, and Luis Cueto-Felgueroso. "Geomechanical Constraints on Hydro-Seismicity: Tidal Forcing and Reservoir Operation." Water 12, no. 10 (2020): 2724. http://dx.doi.org/10.3390/w12102724.

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Understanding the risk associated with anthropogenic earthquakes is essential in the development and management of engineering processes and hydraulic infrastructure that may alter pore pressures and stresses at depth. The possibility of earthquakes triggered by reservoir impoundment, ocean tides, and hydrological events at the Earth surface (hydro-seismicity) has been extensively debated. The link between induced seismicity and hydrological events is currently based on statistical correlations rather than on physical mechanisms. Here, we explore the geomechanical conditions that could allow f

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Fagereng, Å., and A. Beall. "Is complex fault zone behaviour a reflection of rheological heterogeneity?" Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 379, no. 2193 (2021): 20190421. http://dx.doi.org/10.1098/rsta.2019.0421.

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Fault slip speeds range from steady plate boundary creep through to earthquake slip. Geological descriptions of faults range from localized displacement on one or more discrete planes, through to distributed shearing flow in tabular zones of finite thickness, indicating a large range of possible strain rates in natural faults. We review geological observations and analyse numerical models of two-phase shear zones to discuss the degree and distribution of fault zone heterogeneity and effects on active fault slip style. There must be certain conditions that produce earthquakes, creep and slip at

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Barnes, Philip M., Laura M. Wallace, Demian M. Saffer, et al. "Slow slip source characterized by lithological and geometric heterogeneity." Science Advances 6, no. 13 (2020): eaay3314. http://dx.doi.org/10.1126/sciadv.aay3314.

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Slow slip events (SSEs) accommodate a significant proportion of tectonic plate motion at subduction zones, yet little is known about the faults that actually host them. The shallow depth (<2 km) of well-documented SSEs at the Hikurangi subduction zone offshore New Zealand offers a unique opportunity to link geophysical imaging of the subduction zone with direct access to incoming material that represents the megathrust fault rocks hosting slow slip. Two recent International Ocean Discovery Program Expeditions sampled this incoming material before it is entrained immediately down-dip along t

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Seo, Yong Seok, Chang Yong Kim, Kwang Yeom Kim, and Kyoung Mi Lee. "Geomechanical Characterization of Faulted Rock Materials in Korea." Key Engineering Materials 321-323 (October 2006): 328–31. http://dx.doi.org/10.4028/www.scientific.net/kem.321-323.328.

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A faulted rock usually shows the swelling behavior because of clay minerals which consist of the fault gouges. It makes rock mass unstable and threatens the safety of structures built in rock mass. This study was aimed at clarifying characteristics of physical and mechanical properties of faulted rock materials. At first, microstructures and mineralogical composition associated with faulting in the fault gouge zones were analyzed by using X-ray diffractometry (XRD) and SEM microphotographs. Physical properties of the faulted rock materials from fields were measured in the laboratory. It is wel

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Kassym, A. E., V. S. Portnov, M. B. Mynbayev, N. S. Askarova, and А. N. Yessendossova. "Criteria and signs of lead-zinc mineralization within the Maityubinsky anticlinorium." Kompleksnoe Ispolʹzovanie Mineralʹnogo syrʹâ/Complex Use of Mineral Resources/Mineraldik Shikisattardy Keshendi Paidalanu 330, no. 3 (2023): 68–75. http://dx.doi.org/10.31643/2024/6445.30.

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The paper presents research work to establish genetic characteristics of lead-zinc mineralization in the Ulytau-Arganatinsky structural-facial zone. Expanding the mineral resource base of Central Kazakhstan is one of the most urgent tasks because selecting the criteria and characteristics determines the aspects of prospecting and exploration work, as well as their results, which is the goal. In this regard, the following tasks are being solved: identifying the geodynamic position, the genesis of mineralization, the connection of the rock's physical properties with geophysical anomalies, as wel

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Zhu, Danping, Xuewei Liu, and Shaobin Guo. "Reservoir Formation Model and Main Controlling Factors of the Carboniferous Volcanic Reservoir in the Hong-Che Fault Zone, Junggar Basin." Energies 13, no. 22 (2020): 6114. http://dx.doi.org/10.3390/en13226114.

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The Hong-Che Fault Zone is one of the important oil and gas enrichment zones in the Junggar Basin, especially in the Carboniferous. In recent five years, it has been proven that the Carboniferous volcanic rock has 140 million tons of oil reserves, and has built the Carboniferous volcanic reservoir with a capacity of million tons. Practice has proven that the volcanic rocks in this area have great potential for oil and gas exploration and development. To date, Carboniferous volcanic reservoirs have been discovered in well areas such as Che 32, Che 47, Che 91, Chefeng 3, Che 210, and Che 471. Th

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Dissertations / Theses on the topic "Physical properties of fault zones"

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Heermance, Richard V. "Geometry and Physical Properties of the Chelungpu Fault, Taiwan, and Their Effect on Fault Rupture." DigitalCommons@USU, 2002. https://digitalcommons.usu.edu/etd/6720.

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Rupture of the Chelungpu fault during the September 21, 1999, 7.6 Mwearthquake in Taiwan caused a 90-Jr,m-long surface rupture with variable displacement along strike. Analysis of core from two holes drilled through the fault zone, combined with geologic mapping and detailed investigation from three outcrops, define the fault geometry and physical properties of the Chelungpu fault in its northern and southern regions. In the northern region, the fault dips 45-60° east parallel to bedding and consists of a narrow (1-20 cm) core of dark-gray, sheared clay gouge at the base of a 30-50 m zone of i

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Tadokoro, Keiichi. "Physical Properties of Fault Zone in the Postseismic Stage and its Temporal Change." 京都大学 (Kyoto University), 2000. http://hdl.handle.net/2433/181125.

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Flores, Cuba Joseph M. "Earthquake rupture around stepovers in a brittle damage medium." Electronic Thesis or Diss., Sorbonne université, 2023. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2023SORUS301.pdf.

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Les systèmes de failles décrochantes sont constitués d’une variété de complexités géométriques telles que des branchements de failles, des plis et des zones de relais. En particulier, la présence d’une structure de relais peut fortement déterminer la taille finale de la rupture sismique. Ainsi, comprendre la dynamique d’une rupture à travers une telle complexité est crucial pour l’évaluation des risques sismiques. Quelques études ont examiné cette question dans le contexte d’un milieu élastique linéaire. Cependant, lors d’un séisme, des zones d’endommagement sont générées, notamment aux extrém

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Lefèvre, Mélody. "Propriétés structurales, pétro-physiques et circulations de fluides au sein d'une zone de failles dans les argiles." Thesis, Aix-Marseille, 2016. http://www.theses.fr/2016AIXM4320/document.

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Les zones de failles concentrent la migration de fluides et la déformation dans la croûte supérieure. Les propriétés hydrauliques des formations argileuses en font des excellents sites de stockage et des roches mères performants. Les zones de failles peuvent jouer deux rôles contraires dans la circulation de fluides, soit elles s’expriment sous forme de drains, soit elles constituent une barrière, et souvent les deux rôles sont combinés au sein d’une même zone de failles. Les processus de migration des fluides dans les zones de failles affectant les argiles sont peu connus. Cette étude s’est f

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Kelly, Christina. "Understanding seismic properties of fault zones." Thesis, University of Liverpool, 2014. http://livrepository.liverpool.ac.uk/17861/.

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Fault zone properties at depth are often inferred from seismic properties such as seismic velocities and attenuation. An understanding of how fault zone properties and processes influence seismic measurements is required for successful interpretations to be made. As fault zones are heavily fractured and often fluid-rich areas, a knowledge of the influences of cracking and fluid content on seismic measurements is needed. This will allow better interpretation of fault zone properties and how they may change at the time of an earthquake. Research presented in this thesis is concentrated on two re

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Mitchell, Thomas Matthew. "The fluid flow properties of fault damage zones." Thesis, University of Liverpool, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.485852.

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Quantification of the fluid flow properties of the Earth's crust is an essential precursor to the understanding of a wide range of geological processes, including earthquake generation and crustal strength, and the recovery of natural resources. Faults playa key role in the migration of fluids around the ;Earth's crust, and therefore the fluid flow properties of fractured rocks and how these properties evolve with time are of major importance. This thesis aims to improve our understanding of the hydraulic transport properties of large fault zones by presenting a large dataset of detailed field

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Childs, Conrad James. "The structure and hydraulic properties of fault zones." Thesis, University of Liverpool, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.367208.

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Fondriest, Michele. "Structure and mechanical properties of seismogenic fault zones in carbonates." Doctoral thesis, Università degli studi di Padova, 2014. http://hdl.handle.net/11577/3424540.

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In many seismically active areas (e.g. Italy, Greece) earthquakes, sometimes destructive, nucleate within (aftershocks surely do) and propagate through carbonates in the upper crust (e.g. L’Aquila earthquake, 2009, Mw 6.1). Seismology, geophysics and geodesy furnish key parameters related to the earthquake source (e.g. seismic moment, static stress drop, radiated energy) but lack sufficient resolution to constrain detailed three-dimensional fault zone geometry and coseismic on- and off-fault deformation processes at scales relevant to earthquake physics. In this thesis it is proposed to stud

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Haines, Thomas J. "The evolution of petrophysical properties across carbonate hosted normal fault zones." Thesis, University of Aberdeen, 2014. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=225315.

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Jeanne, Pierre. "Architectural, petrophysical and hydromechanical properties of fault zones in fractured-porous rocks : compared studies of a moderate and a mature fault zones (France)." Nice, 2012. http://www.theses.fr/2012NICE4016.

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Bien que les zones de failles représentent un très petit volume de la croute terrestre, elles influencent grandement ses propriétés hydromécaniques. Ce travail compare des analyses multidisciplinaires, de hautes précisions, de deux zones de failles aux propriétés contrastées : l’une est une zone de failles mature de plusieurs kilomètres de long, l’autre s’étend seulement sur quelques centaines de mètres. Leurs propriétés architecturales, hydromécaniques et de résistance mécanique ont été caractérisées dans le but d’améliorer la compréhension des couplages entre l’évolution de leurs propriétés

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Books on the topic "Physical properties of fault zones"

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Minor, Scott A. Regional survey of structural properties and cementation patterns of fault zones in the northern part of the Albuquerque basin, New Mexico--implications for ground-water flow. U.S. Geological Survey, 2006.

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(Editor), David D. Bruhn, and Luigi Burlini (Editor), eds. High-Strain Zones: Structure and Physical Properties. Geological Society of London, 2005.

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J, Wibberley C. A., ed. The internal structure of fault zones: Implications for mechanical and fluid-flow properties. Geological Society, 2008.

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Ben-Zion, Yehuda, and Antonio Rovelli. Properties and Processes of Crustal Fault Zones: Volume I. Birkhäuser, 2014.

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Ben-Zion, Yehuda, and Antonio Rovelli. Properties and Processes of Crustal Fault Zones: Volume II. Springer, 2015.

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Book chapters on the topic "Physical properties of fault zones"

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Yamashita, Teruo, and Akito Tsutsumi. "Fluid-Flow Properties of Fault Zones." In Involvement of Fluids in Earthquake Ruptures. Springer Japan, 2017. http://dx.doi.org/10.1007/978-4-431-56562-8_3.

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Rácz, Zoltán. "Continuum Description of Active Zones." In Fractals’ Physical Origin and Properties. Springer US, 1989. http://dx.doi.org/10.1007/978-1-4899-3499-4_8.

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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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Rockwell, Thomas, Matthew Sisk, Gary Girty, Ory Dor, Neta Wechsler, and Yehuda Ben-Zion. "Chemical and Physical Characteristics of Pulverized Tejon Lookout Granite Adjacent to the San Andreas and Garlock Faults: Implications for Earthquake Physics." In Mechanics, Structure and Evolution of Fault Zones. Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0138-2_9.

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Hsu, Ya-Ju, Jean-Philippe Avouac, Shui-Beih Yu, Chien-Hsin Chang, Yih-Min Wu, and Jochen Woessner. "Spatio-temporal Slip, and Stress Level on the Faults within the Western Foothills of Taiwan: Implications for Fault Frictional Properties." In Mechanics, Structure and Evolution of Fault Zones. Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0138-2_14.

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Ogita, N., Y. Kito, T. Kimizu, and R. Yatabe. "Physical properties of clay from landslides in large fracture zones." In Slope Stability Engineering. Routledge, 2021. http://dx.doi.org/10.1201/9780203739600-105.

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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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Bouckaert, L. P., R. Smoluchowski, and E. P. Wigner. "Theory of the Brillouin Zones and Symmetry Properties of Wave Functions in Crystals." In Part I: Physical Chemistry. Part II: Solid State Physics. Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-642-59033-7_40.

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Ruzhich, Valery V., and Evgeny V. Shilko. "A New Method for Seismically Safe Managing of Seismotectonic Deformations in Fault Zones." In Springer Tracts in Mechanical Engineering. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-60124-9_3.

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AbstractThe authors outline the results of long-term interdisciplinary research aimed at identifying the possibility and the methods of controlling tangential displacements in seismically dangerous faults to reduce the seismic risk of potential earthquakes. The studies include full-scale physical and numerical modeling of P-T conditions in the earth’s crust contributing to the initiation of displacement in the stick-slip regime and associated seismic radiation. A cooperation of specialists in physical mesomechanics, seismogeology, geomechanics, and tribology made it possible to combine and generalize data on the mechanisms for the formation of the sources of dangerous earthquakes in the highly stressed segments of faults. We consider the prospect of man-caused actions on the deep horizons of fault zones using powerful shocks or vibrations in combination with injecting aqueous solutions through deep wells to manage the slip mode. We show that such actions contribute to a decrease in the coseismic slip velocity in the fault zone, and, therefore, cause a decrease in the amplitude and energy of seismic vibrations. In conclusion, we substantiate the efficiency of the use of combined impacts on potentially seismically hazardous segments of fault zones identified in the medium-term seismic prognosis. Finally, we discuss the importance of the full-scale validation of the proposed approach to managing the displacement regime in highly-stressed segments of fault zones. Validation should be based on large-scale tests involving advanced technologies for drilling deep multidirectional wells, injection of complex fluids, and localized vibrational or pulse impacts on deep horizons.

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Hashimoto, Chihiro, and Mitsuhiro Matsu’ura. "3-D Simulation of Earthquake Generation Cycles and Evolution of Fault Constitutitve Properties." In Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part II. Birkhäuser Basel, 2002. http://dx.doi.org/10.1007/978-3-0348-8197-5_2.

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Conference papers on the topic "Physical properties of fault zones"

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Vaas, Christian, Marc Roeschlin, Panos Papadimitratos, and Ivan Martinovic. "Poster: Tracking Vehicles Through Encrypted Mix-Zones Using Physical Layer Properties." In 2018 IEEE Vehicular Networking Conference (VNC). IEEE, 2018. http://dx.doi.org/10.1109/vnc.2018.8628387.

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Michie, E. A. H., T. J. Haines, D. Healy, J. Neilson, G. I. Alsop, and N. E. Timms. "Fracture Patterns in Carbonate Fault Zones and their Influence on Petrophysical Properties." In 3rd EAGE International Conference on Fault and Top Seals. EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20143034.

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ter Heege, J. H., B. B. T. Wassing, S. B. Giger, and M. B. Clennell. "Numerical Modelling of the Mechanical and Fluid Flow Properties of Fault Zones – Implications for Fault Seal Analysis." In 2nd EAGE International Conference on Fault and Top Seals - From Pore to Basin Scale 2009. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609.20147195.

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Al-Jumah, Ali, Melih Gokmen, Ameera Harrasi, Ibrahim Abri, Salim Buwaiqi, and Gerardo Urdaneta. "Field Application of the Autonomous Inflow Control Device AICD for Optimized Heavy Oil Production in South Sultanate of Oman." In SPE Conference at Oman Petroleum & Energy Show. SPE, 2022. http://dx.doi.org/10.2118/200279-ms.

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Abstract This paper summarizes the results and learnings from the Autonomous Inflow Control Device (AICD) deployment and installation in multiple heavy oil fields in south Oman, allowing for swift utilization in other fields with similar characteristics. Those AICDs were mainly deployed and tested in those oil fields comprehensively, in horizontal producers, and the results were supported by rigorous lab tests was conducted to understand their behavior. This paper is a continuation of the work in reference [1]. In recent decades, horizontal drilling for producing wells became a widely known an

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Camus, A. Sánchez, R. Ramos, and L. Bianchi. "Latest Advances in 3-D and 4-D FEM Simulation for Comprehensive Geomechanical and Geophysical Analysis of Unconventional Reservoirs, from Field Data to Numerical Models: Case Study Fm. Vaca Muerta, Argentina." In Offshore Technology Conference Brasil. OTC, 2023. http://dx.doi.org/10.4043/32775-ms.

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Abstract The prime goal of the comprehensive characterization of unconventional reservoirs (organic-rich mudrocks) is to build 3-D and 4-D FEM numerical models for geomechanical and geophysical studies, such as seismic full-wave propagation, AVO or AVAz analysis, seismic inversion, well stability, hydraulic fracture propagation, cement shield and casing integrity, well to well interaction, choke management for optimal well production, tests for different landing zones, fault and layer reactivation risk cubes and other geomechanical attributes. The current technologies for the acquisition and p

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Aubert, I., P. Léonide, J. Lamarche, and R. Salardon. "Diagenetic Impact on Polyphase Fault Zones Drain Properties in Micro-Porous Carbonates (Urgonian – SE France)." In Fifth International Conference on Fault and Top Seals. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201902326.

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Feijoo Calle, Ernesto Patricio, Andrés Nicolás Aguirre Larriva, and Bernardo Andrés Feijoo Guevara. "Influence zones generated by physical properties for the characterization of rock material in the field." In VIII Congreso Internacional de Investigación REDU. Medwave, 2022. http://dx.doi.org/10.5867/medwave.2022.s1.ci29.

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Joshi, Heet S., Tejas Turakhia, Mehul R. Pandya, and Rajesh R. Iyer. "Investigation of Optical and Physical Properties of Aerosol Over Different Sub-Zones of Ahmedabad, India." In 2023 IEEE India Geoscience and Remote Sensing Symposium (InGARSS). IEEE, 2023. http://dx.doi.org/10.1109/ingarss59135.2023.10490420.

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Zhang, Tiansheng, and Haiying Huang. "Physical Properties and Fracture Network Characteristics of Mafic and Ultramafic Rocks." In 57th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2023. http://dx.doi.org/10.56952/arma-2023-0951.

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ABSTRACT Mineral carbon storage in mafic and ultramafic rocks is a novel concept for CO2 sequestration. In contrast to carbon sequestration in sedimentary formations, where structural and residual trappings are the primary mechanisms of storage, solubility and mineral trappings are expected to be the dominant storage mechanisms in mafic and ultramafic rocks. Mafic and ultramafic rocks are rich in calcium, magnesium and iron. Mineral carbonation occurs when these rocks are exposed to an environment with CO2 and water. Feasibility of mineral carbon storage has been demonstrated in field trials i

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Agosta, Fabrizio, Manika Prasad, and Atilla Aydin. "Rock physical properties of carbonate fault rocks, Fucino Basin (central Italy)." In SEG Technical Program Expanded Abstracts 2004. Society of Exploration Geophysicists, 2004. http://dx.doi.org/10.1190/1.1845166.

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Reports on the topic "Physical properties of fault zones"

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Shroba, R. R., D. R. Muhs, and J. N. Rosholt. Physical properties and radiometric age estimates of surficial and fracture-fill deposits along a portion of the Carpetbag fault system, Nevada Test Site, Nye County, Nevada. Office of Scientific and Technical Information (OSTI), 1988. http://dx.doi.org/10.2172/6970125.

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Hayward, N., and V. Tschirhart. A comparison of 3-D inversion strategies in the investigation of the 3-D density and magnetic susceptibility distribution in the Great Bear Magmatic Zone, Northwest Territories. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/331954.

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The inversion of new compilations of aeromagnetic data and gravity data are employed to investigate the 3-D physical property (magnetic susceptibility and density) distribution within the Great Bear magmatic zone. The application of two different software suites (Geosoft VOXI and UBC GIF MAG3D and GRAV3D) affords a comparison of approaches and results. The magnetic susceptibility results are broadly compatible, but Geosoft VOXI enabled more detailed definition of shallow sources. The density results were markedly different in how the model responded to the low-resolution gravity data in charac

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Dinovitzer, Aaron. PR-214-144500-R05 Weld Hydrogen Cracking Susceptibility Characterization. Pipeline Research Council International, Inc. (PRCI), 2018. http://dx.doi.org/10.55274/r0011495.

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Hydrogen cracking has been and continues to be observed in both heat-affected zones and weld metals. High carbon equivalent weldment heat-affected zones (HAZ) combined with rapid cooling have been related to the development of hydrogen cracking susceptible microstructures. Weld metal cracking is observed in both high and low strength weldments and is a particular concern for root passes due to the use of cellulosic electrodes, parent metal dilution, applied load, and weld fault stress riser effects promoting cracking. The risk of HAZ and weld cracking are increased for repair and in-service we

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