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- W1753329270 abstract "Structurally thickened, buckled, and brecciated chert beds form an important pathway for bedding parallel fluid migration in the Monterey Formation of California. Pure opalCT and quartz cherts formed significantly before the corresponding silica phase changes in associated porcelanite or siliceous mudstone in the Monterey. This early formation of extremely brittle chert took place within more porous, ductilely deforming, and low permeability host rock. When strained by tectonic, compactional, or downslope stresses, the chert fractured or brecciated, increasing bedding parallel permeability by several orders of magnitude along the brecciated beds. Repeated cycles of embrittlement /brecciation/ permeability enhancement/recementation permitted between 2,500 and 20,000 volumes of water to passed through many fractured chert beds, ultimately contributing 5% - 40% of the volume of the rock as void-filling silica cement. This high degree of brecciation and cementation was commonly obscured by late diagenetic recrystallization. If oil was mobilized and introduced into the breccias prior to complete cementation, however, then the cherts can serve as highly permeabl e fractured petroleum reservoirs." @default.
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- W1753329270 date "1998-01-01" @default.
- W1753329270 modified "2023-09-25" @default.
- W1753329270 title "RELATIONSHIPS BETWEEN SILICA DIAGENESIS, DEFORMATION, AND FLUID FLOW IN MONTEREY FORMATION CHERTS, SANTA MARIA BASIN, CALIFORNIA." @default.
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