Literatura científica selecionada sobre o tema "Physical properties of fault zones"
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Artigos de revistas sobre o assunto "Physical properties of fault zones"
Verberne, Berend A., Oliver Plümper e Christopher J. Spiers. "Nanocrystalline Principal Slip Zones and Their Role in Controlling Crustal Fault Rheology". Minerals 9, n.º 6 (28 de maio de 2019): 328. http://dx.doi.org/10.3390/min9060328.
Texto completo da fonteGibson, Richard G. "Physical character and fluid-flow properties of sandstone-derived fault zones". Geological Society, London, Special Publications 127, n.º 1 (1998): 83–97. http://dx.doi.org/10.1144/gsl.sp.1998.127.01.07.
Texto completo da fonteGuillou-Frottier, Laurent, Hugo Duwiquet, Gaëtan Launay, Audrey Taillefer, Vincent Roche e 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, n.º 4 (26 de agosto de 2020): 1571–95. http://dx.doi.org/10.5194/se-11-1571-2020.
Texto completo da fonteZoback, M., S. Hickman e W. Ellsworth. "Scientific Drilling Into the San Andreas Fault Zone – An Overview of SAFOD's First Five Years". Scientific Drilling 11 (1 de março de 2011): 14–28. http://dx.doi.org/10.5194/sd-11-14-2011.
Texto completo da fontePampillón, Pedro, David Santillán, Juan Carlos Mosquera e Luis Cueto-Felgueroso. "Geomechanical Constraints on Hydro-Seismicity: Tidal Forcing and Reservoir Operation". Water 12, n.º 10 (29 de setembro de 2020): 2724. http://dx.doi.org/10.3390/w12102724.
Texto completo da fonteFagereng, Å., e 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, n.º 2193 (fevereiro de 2021): 20190421. http://dx.doi.org/10.1098/rsta.2019.0421.
Texto completo da fonteBarnes, Philip M., Laura M. Wallace, Demian M. Saffer, Rebecca E. Bell, Michael B. Underwood, Ake Fagereng, Francesca Meneghini et al. "Slow slip source characterized by lithological and geometric heterogeneity". Science Advances 6, n.º 13 (março de 2020): eaay3314. http://dx.doi.org/10.1126/sciadv.aay3314.
Texto completo da fonteSeo, Yong Seok, Chang Yong Kim, Kwang Yeom Kim e Kyoung Mi Lee. "Geomechanical Characterization of Faulted Rock Materials in Korea". Key Engineering Materials 321-323 (outubro de 2006): 328–31. http://dx.doi.org/10.4028/www.scientific.net/kem.321-323.328.
Texto completo da fonteKassym, A. E., V. S. Portnov, M. B. Mynbayev, N. S. Askarova e 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, n.º 3 (7 de dezembro de 2023): 68–75. http://dx.doi.org/10.31643/2024/6445.30.
Texto completo da fonteZhu, Danping, Xuewei Liu e Shaobin Guo. "Reservoir Formation Model and Main Controlling Factors of the Carboniferous Volcanic Reservoir in the Hong-Che Fault Zone, Junggar Basin". Energies 13, n.º 22 (21 de novembro de 2020): 6114. http://dx.doi.org/10.3390/en13226114.
Texto completo da fonteTeses / dissertações sobre o assunto "Physical properties of fault zones"
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.
Texto completo da fonteTadokoro, 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.
Texto completo da fonteFlores, 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.
Texto completo da fonteStrike-slip fault systems consist of a variety of geometrical complexities like branches, kinks and step-overs. Especially, the presence of a step-over structure can strongly determine the final size of the earthquake rupture. Thus understanding the dynamics of a rupture through such a complexity is crucial for seismic hazard assessment. A few studies have looked at this question within the context of a linear elastic medium. However, during an earthquake off-fault damage is generated, especially at the ends of a fault, which significantly changes the overall dynamics of a rupture. Using a micromechanical model, that accounts for crack growth and opening and its impact on the dynamic evolution of elastic moduli, we evaluate how dynamic off-fault damage can affect the capability of a rupture to navigate through step-over fault structures. We show that, sometimes, accounting for this energy sink, off-damage suppresses the ability of the rupture to jump from one fault to another. Whereas, in some specific cases, the dynamically created low-velocity zone may aid the rupture to jump on the secondary fault. Combing this numerical study with an analytical analysis we set the contours for a systematic approach useful for earthquake hazard assessments
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.
Texto completo da fonteFault zones concentrate fluids migration and deformations in the upper crust. The shale hydraulic properties make them excellent storage sites and hydrocarbon reservoirs/source rocks. Fault zones can play two roles in the fluid circulation; drains or barriers, in general, both roles are combined within the same fault zone. What are the conditions that promote the fluid circulation along the fault zones in shales and what are the fault zone impacts on the formation properties are relatively poorly explored key questions. This study focused on characterizing the relationships between fault architecture, paleo-fluid as well as current fluid circulations through the analysis of fault calcite mineralization, injection tests and petrophysical properties conducted on a fault zone outcropping underground in the Tournemire research laboratory nested in the Toarcian shale. The fault zone structure was characterized using boreholes data and reconstructed in 3D through modeling to define different deformation facies. No clear facies organization is observed, a fault core and a fault damage zone being difficult to define as it is in hard rocks. The intact, fractured and breccia facies are characterized by a porosity of 9.5-13.5, 10-15 and 13-21%. Large fluid flowrate concentrated along a few “channels” located at the breccia boundaries and in the secondary fault zones that displayed fractured facies and limited breccia fillings. Detailed microstructural and geochemical analysis at the breccia/fractured zones interface revealed that fluids circulated out of the main shear zones, in micro-more or less inherited fractures highlighting a decoupling between fault slip and fluid migrations
Kelly, Christina. "Understanding seismic properties of fault zones". Thesis, University of Liverpool, 2014. http://livrepository.liverpool.ac.uk/17861/.
Texto completo da fonteMitchell, 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.
Texto completo da fonteChilds, 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.
Texto completo da fonteFondriest, 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.
Texto completo da fonteIn molte regioni sismiche dell’area Mediterranea, tra cui l’Italia e la Grecia, gran parte dei terremoti, anche distruttivi, enucleano e propagano in sequenze di rocce carbonatiche della crosta superiore (terremoto dell’Aquila, 2009, Mw 6.1). Questo è vero soprattutto per le sequenze di foreshock e aftershock. Le indagini sismologiche, geofisiche e geodetiche forniscono dei parametri fondamentali per la caratterizzazione delle sorgenti sismiche (momento sismico, caduta di sforzo statico, energia elastica irradiata) ma non hanno risoluzione spaziale sufficiente per descrivere in maniera dettagliata la geometria delle sorgenti sismiche e i processi chimico-fisici attivi nelle zone di faglia durante un terremoto. Questi aspetti limitano fortemente la nostra conoscenza della fisica dei terremoti. In questa tesi la struttura interna e le proprietà meccaniche di zone di faglia sismogenetiche in rocce carbonatiche sono state studiate utilizzando un approccio multidisciplinare e complementare rispetto a quello classico basato su dati sismologici principalmente ricavati dall’inversione delle onde sismiche. I metodi utilizzati sono: (i) il rilevamento strutturale di dettaglio di zone di faglia esumate in carbonati con tecniche di terreno e di telerilevamento (ad es. utilizzo di un drone per ottenere immagini ad alta risoluzione di grandi affioramenti), (ii) la realizzazione di prove meccaniche su roccia (e polveri di roccia) in condizioni di deformazione rilevanti per il ciclo sismico (utilizzo di apparati di tipo rotary, pressa uniassiale e Split Hopkinson Pressure Bar), (iii) lo studio mineralogico-microstrutturale (microscopia ottica e a scansione elettronica, microsonda elettronica, diffrazione a raggi X su polveri, catodoluminescenza, microtomografia a raggi X, interferometria in luce bianca, analisi di immagine) di rocce di faglia naturali e sperimentali per vincolare i processi chimico-fisici attivi in carbonati durante un terremoto. Sono state selezionate due zone di faglia in dolomie: la zona di faglia del Passo della Borcola (BPFZ) e la zona di faglia di Foiana (FFZ). Entrambe le zone di faglia sono esumate da profondità < 3 km e affiorano nel settore delle Alpi Meridionali (Italia). L’architettura interna delle due zone di faglia è fortemente controllata dalla riattivazione di strutture ereditate come sistemi di giunti a scala regionale e superfici di strato. La BPFZ è una faglia secondaria trascorrente appartenente al sistema della Linea Schio-Vicenza. La presenza all’interno della BPFZ di zone di scivolamento estremamente localizzate e spesso organizzate in livelli cataclastici ed ultracataclastici con bordi irregolari (a lobi e cuspidi), iniettati lungo fratture estensionali e caratterizzati da una forte selezione granulometrica ha suggerito l’attivazione di fenomeni di fluidizzazione durante la propagazione di rotture sismiche in un ambiente ricco in fluidi. La FFZ è una faglia transpressiva sinistra a scala regionale che presenta sistematiche variazioni nella propria struttura interna (e.g. spessore della zona di faglia, orientazione e cinematica delle faglie minori) lungo la direzione e l’immersione della faglia. La zona di faglia esposta è caratterizzata dalla presenza di dolomie frantumate senza evidenze significative di deformazione per taglio (dolomie frantumate in-situ) associate a faglie con piccoli rigetti (< 0.5 m) e superfici a specchio con clasti troncati. L’assenza di vene o fratture sigillate indica che la fagliazione è avvenuta in un ambiente povero in fluidi. L’origine delle faglie con superfici a specchio e delle dolomie frantumate in-situ della FFZ è stata investigata attraverso esperimenti eseguiti (1) con un apparato di tipo rotary imponendo basse ed alte velocità (0.0001-1 m/s) di scivolamento su polveri di dolomia e (2) con un pressa uniassiale e una Split Hopkinson Pressure Bar imponendo basse ed alte velocità di deformazione (quasi-statiche 10-3 s-1, dinamiche > 50 s-1) su cilindri di dolomia. Applicando le condizioni di sforzo normale e rigetto stimate per le faglie della FFZ, superfici a specchio simili a quelle naturali in termini di rugosità delle superfici e di microstrutture (presenza di clasti troncati lungo le superfici di faglia), sono state prodotte negli esperimenti di tipo rotary solo a velocità di scivolamento cosismiche (v ≥ 0.1 m/s). Inoltre dolomie frantumate in-situ con microstrutture simili a quelle descritte lungo la FFZ (frammenti di roccia con dimensioni fino a qualche millimetro allungati nella direzione di applicazione del carico e zone di microfratturazione incipiente) sono state prodotte negli esperimenti con la Split Hopkinson Pressure Bar solo a ratei di deformazione > 200 s-1 : tali ratei di deformazione sono in genere associati alle perturbazioni di sforzo dovute al passaggio di una rottura sismica. Pertanto l’associazione di dolomie frantumate in-situ tagliate da faglie discrete con superfici a specchio è stata interpretata come il risultato della propagazione di rotture sismiche nelle porzioni superficiali della FFZ. Infine, a livello qualitativo, la complessità strutturale delle due zone di faglia studiate in termini di geometria del network di faglie e fratture, distribuzione spaziale delle rocce di faglia, orientazione e cinematica delle faglie, è confrontabile sia con la distribuzione del danneggiamento di faglia predetta da simulazioni di rotture sismiche, sia con la struttura di sorgenti sismogenetiche attuali in carbonati desunta da osservazioni sismologiche
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.
Texto completo da fonteJeanne, 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.
Texto completo da fonteAlthough fault zones represent a very small volume of the crust, they highly influence the crust’s mechanical and fluid flows properties. This work compares high definition trans-disciplinary analyses of two fault zones with highly contrasted properties. One is a mature fault zone of plurikilometer length, and the other is a small fault zone of a few hundred meters length. We have characterized the architectural, hydromechanical and strength properties of these faults to improve the understanding of the coupling between fault zones hydromechanical properties and their potential activation. A protocol to characterize in the field (on outcropping segments) the faults hydraulic and mechanical properties has been conducted through the coupling of micro-structural analyses, detailed rock physical descriptions at the rock mass several scales. The two studied fault zones despite their different sizes display some similarities. Both show a strong coupling between the fault zone diagenetic history, the initial properties of the sedimentary layers and the fault zone current hydraulic and mechanical properties. We show that the most important parameter governing the hydromechanical behaviors of fault zones is the continuity of the damage zones. A mature fault zone will have a relatively continuous damage zone while a small fault zone will contain a more heterogeneous damage zone characterized by an alternation of fractured and un-fractured layers. These architectural contrasts of damage zones also depend on the initial intact rock properties of the sedimentary series. Contrasted initial intact rock strengths (σc) induce contrasted strain accommodation mechanisms in the fault zone compartments, and an associated fault zone architecture that displays large thickness variations, characterized by alternate high-permeable-low-stiff and low-permeable-high-stiff layers in the damage zone
Livros sobre o assunto "Physical properties of fault zones"
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. Reston, Va: U.S. Geological Survey, 2006.
Encontre o texto completo da fonte(Editor), David D. Bruhn, e Luigi Burlini (Editor), eds. High-Strain Zones: Structure and Physical Properties. Geological Society of London, 2005.
Encontre o texto completo da fonteJ, Wibberley C. A., ed. The internal structure of fault zones: Implications for mechanical and fluid-flow properties. London: Geological Society, 2008.
Encontre o texto completo da fonteBen-Zion, Yehuda, e Antonio Rovelli. Properties and Processes of Crustal Fault Zones: Volume I. Birkhäuser, 2014.
Encontre o texto completo da fonteBen-Zion, Yehuda, e Antonio Rovelli. Properties and Processes of Crustal Fault Zones: Volume II. Springer, 2015.
Encontre o texto completo da fonteCapítulos de livros sobre o assunto "Physical properties of fault zones"
Yamashita, Teruo, e Akito Tsutsumi. "Fluid-Flow Properties of Fault Zones". In Involvement of Fluids in Earthquake Ruptures, 51–71. Tokyo: Springer Japan, 2017. http://dx.doi.org/10.1007/978-4-431-56562-8_3.
Texto completo da fonteRácz, Zoltán. "Continuum Description of Active Zones". In Fractals’ Physical Origin and Properties, 193–203. Boston, MA: Springer US, 1989. http://dx.doi.org/10.1007/978-1-4899-3499-4_8.
Texto completo da fonteFinzi, Yaron, Elizabeth H. Hearn, Yehuda Ben-Zion e Vladimir Lyakhovsky. "Structural Properties and Deformation Patterns of Evolving Strike-slip Faults: Numerical Simulations Incorporating Damage Rheology". In Mechanics, Structure and Evolution of Fault Zones, 1537–73. Basel: Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0138-2_2.
Texto completo da fonteRockwell, Thomas, Matthew Sisk, Gary Girty, Ory Dor, Neta Wechsler e 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, 1725–46. Basel: Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0138-2_9.
Texto completo da fonteHsu, Ya-Ju, Jean-Philippe Avouac, Shui-Beih Yu, Chien-Hsin Chang, Yih-Min Wu e 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, 1853–84. Basel: Birkhäuser Basel, 2009. http://dx.doi.org/10.1007/978-3-0346-0138-2_14.
Texto completo da fonteOgita, N., Y. Kito, T. Kimizu e R. Yatabe. "Physical properties of clay from landslides in large fracture zones". In Slope Stability Engineering, 1229–32. London: Routledge, 2021. http://dx.doi.org/10.1201/9780203739600-105.
Texto completo da fonteBilek, Susan L., e 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, 433–56. Basel: Birkhäuser Basel, 1999. http://dx.doi.org/10.1007/978-3-0348-8679-6_3.
Texto completo da fonteBouckaert, L. P., R. Smoluchowski e 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, 416–25. Berlin, Heidelberg: Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-642-59033-7_40.
Texto completo da fonteRuzhich, Valery V., e Evgeny V. Shilko. "A New Method for Seismically Safe Managing of Seismotectonic Deformations in Fault Zones". In Springer Tracts in Mechanical Engineering, 45–66. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-60124-9_3.
Texto completo da fonteHashimoto, Chihiro, e 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, 2175–99. Basel: Birkhäuser Basel, 2002. http://dx.doi.org/10.1007/978-3-0348-8197-5_2.
Texto completo da fonteTrabalhos de conferências sobre o assunto "Physical properties of fault zones"
Vaas, Christian, Marc Roeschlin, Panos Papadimitratos e 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.
Texto completo da fonteMichie, E. A. H., T. J. Haines, D. Healy, J. Neilson, G. I. Alsop e 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. Netherlands: EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20143034.
Texto completo da fonteter Heege, J. H., B. B. T. Wassing, S. B. Giger e 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.
Texto completo da fonteAl-Jumah, Ali, Melih Gokmen, Ameera Harrasi, Ibrahim Abri, Salim Buwaiqi e 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.
Texto completo da fonteCamus, A. Sánchez, R. Ramos e 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.
Texto completo da fonteAubert, I., P. Léonide, J. Lamarche e 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.
Texto completo da fonteFeijoo Calle, Ernesto Patricio, Andrés Nicolás Aguirre Larriva e 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.
Texto completo da fonteJoshi, Heet S., Tejas Turakhia, Mehul R. Pandya e 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.
Texto completo da fonteZhang, Tiansheng, e 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.
Texto completo da fonteAgosta, Fabrizio, Manika Prasad e 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.
Texto completo da fonteRelatórios de organizações sobre o assunto "Physical properties of fault zones"
Shroba, R. R., D. R. Muhs e 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), julho de 1988. http://dx.doi.org/10.2172/6970125.
Texto completo da fonteHayward, N., e 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.
Texto completo da fonteDinovitzer, Aaron. PR-214-144500-R05 Weld Hydrogen Cracking Susceptibility Characterization. Chantilly, Virginia: Pipeline Research Council International, Inc. (PRCI), julho de 2018. http://dx.doi.org/10.55274/r0011495.
Texto completo da fonte