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- W2495302166 abstract "Abstract Subduction zones where old oceanic plate underthrusting occurs are characterized by thick pelagic sediments originating from planktonic ooze as well as cold thermal conditions. For a better understanding of dehydration from pelagic sediments and fluid behavior, which would play a key role in controlling the dynamics in the shallow portion of the subduction zone, as observed in the 2011 Tohoku earthquake and tsunami, we investigate cherts in a Jurassic accretionary complex in Japan. The microstructure and microchemistry of these cherts indicate dissolution of SiO 2 from a pressure solution seam and precipitation of SiO 2 to the “white chert layer,” which would act as a fluid conduit. The amount of water necessary to precipitate SiO 2 in the white chert is ~ 10 2 times larger than that produced by compaction and silica/clay diagenesis. Other fluid sources, such as hydrated oceanic crust or oceanic mantle, are necessary to account for this discrepancy in the fluid budget. A large amount of external fluid likely contributed to rising pore pressure along cold plate boundaries." @default.
- W2495302166 created "2016-08-23" @default.
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- W2495302166 date "2016-08-01" @default.
- W2495302166 modified "2023-10-03" @default.
- W2495302166 title "Source and sink of fluid in pelagic siliceous sediments along a cold subduction plate boundary" @default.
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- W2495302166 doi "https://doi.org/10.1016/j.tecto.2016.07.030" @default.
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