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• W2182012766 abstract "The faults in the steeply dipping domain of Hole 863B are situated in a distinct tectonic setting, where an active spreading center is subducting. Early rheological contrasts, arising from primary compositional differences, were enhanced by fluid flow channeled along bedding planes. Several early faults focalized under low effective stresses, parallel to bedding planes. Fluid flow was focused along discrete millimeter to centimeter-scale, branching channels within fault zones and their surroundings, even though the sediments were only partially consolidated. Individual core-scale fault zones accommodate only minor strain but they contain penetrative grain-scale fabrics. These fabrics were generated during a dilation-fluid flow-porosity collapse history, interpreted from textural variations and cross-cutting relations in fault zones. There is no evidence for cataclasis or pressure solution in fault rocks but some dissolution has occurred. A generalized sequence of cementation is represented by early sulfate and clay minerals and zeolites followed by pyrite, carbonate and minor quartz. Carbonate and pyrite cements formed prior to and synchronously with normal faults. Normal faults generally post-date reverse faults and could be related to ridge subduction. The interpreted deformation and cementation histories illustrate the fine-scale porosity (and permeability?) variations caused by linked cementation and deformation in the earliest stages of accretion." @default.
• W2182012766 created "2016-06-24" @default.
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• W2182012766 date "1995-09-01" @default.
• W2182012766 modified "2023-09-24" @default.
• W2182012766 title "Faulting and Fluid Flow in Accreted Sediments: Hole 863B, Chile Triple Junction" @default.
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• W2182012766 doi "https://doi.org/10.2973/odp.proc.sr.141.116.1995" @default.
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