Fault transmissibility in clastic-argillaceous sequences controlled by clay smear evolution (Record no. 187781)

MARC details
000 -LEADER
fixed length control field 02478nab a2200253 4500
008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL
Campo de control de longitud fija 260224s2013 xxu ing
041 ## - IDIOMA
Idioma Inglés
245 00 - TITULO
Título Fault transmissibility in clastic-argillaceous sequences controlled by clay smear evolution
260 ## - PUBLICACION, DISTRIBUCION, ETC
Lugar de publicación, distribución, etc.
Nombre de publicador, distribuidor, etc.
Fecha de publicación, distribución, etc. mayo 2013
270 ## - FECHA DE CARGA
Fecha de carga 24/06/2013 ; 24/06/2013
300 ## - DESCRIPCION FISICA
Otra extensión 26 p. ; 705-731
520 ## - RESUMEN, ETC
Resumen Transcripción del resumen del autor: The continuity of clay smears evolving in sealed direct shear experiments of initially intact sandstone-mudrock sequences was quantified to large displacements up to more than ten times the thickness of the sealing layer. The sample blocks consisted of a preconsolidated clay-rich seal layer, which was embedded and synthetically cemented in quartz sand. The mineralogy and mechanical properties of the clay layer and the reservoir sandstones were varied systematically to mimic a range of natural clastic rock sequences. The fluid-flow response across the fault zone was monitored continuously during deformation using a new type of direct shear cell. The displacement at which seals break down is closely linked to the amount of phyllosilicates in the seal layer. Contrary to expectations, softer seal layers do not seal better than stiff seal layers for a given clay content. In the testing range of normal effective stresses between 4 to 24 MPa (580–3481 psi) covering maximum burial depth conditions of approximately 800 m (2625 ft) to approximately 4 km (2 mi) (assuming normal fault tectonics), a systematic trend is also observed, indicating better smear continuity by increasing the effective normal stress. Predominantly brittle processes such as slicing and wear, and not ductile drag or plastic flow, appear to be responsible for the generation of clay smears. The test results offer the prospect of incorporating critical shale smear factors (i.e., normalized displacement at which seal breakdown occurs) into probabilistic fault seal algorithms that consider important properties that can be measured or estimated, namely, clay content and fault-normal effective stress.
581 ## - ESTADO DE COLECCIÓN
Estado de colección 5
773 0# - CORRECCIÓN
Título AAPG Bulletin
Partes relacionadas 97
942 ## - DESC. DE MATERIAL
Tipo de item KOHA Artículo de Revista
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Giger, Silvio B.
9 (RLIN) 53335
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Apellido, Nombre Clennell, Michael B.
9 (RLIN) 53336
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Apellido, Nombre Ciftci, N. Bozkurt
9 (RLIN) 53337
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Apellido, Nombre Harbers, Craig
9 (RLIN) 53338
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Apellido, Nombre Clark, Peter
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Apellido, Nombre Ricchetti, Mark
9 (RLIN) 53340
Holdings
Biblioteca propietaria Biblioteca actual Fecha de adquisición Inventario Total de préstamos Inventario Fecha de carga Tipo de item KOHA
Biblioteca Alejandro Angel Bulgheroni Biblioteca Alejandro Angel Bulgheroni 06/03/2026 200059924   200059924 06/03/2026 Artículo de Revista


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