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• W3091802355 endingPage "116601" @default.
• W3091802355 startingPage "116601" @default.
• W3091802355 abstract "Non-volcanic tremor (NVT) and episodic slow slip events (SSEs) have been observed below the seismogenic zone of relatively warm subduction zones for the past 20 years. Geophysical and geologic observations show that this portion of the subduction interface is fluid-rich, and many models for these slip behaviors necessitate high pore fluid pressures. However, whether these fluids are sourced from local dehydration reactions in particular lithologies, or require up-dip transport from greater depths is not known. We present thermodynamic models of the petrologic evolution of four lithologies typical of the plate interface (average MORB, seafloor altered MORB, hydrated depleted MORB mantle, and metapelite) along predicted plate boundary pressure–temperature (P-T) paths at several warm subduction segments where NVT and SSEs are observed at depths between 25-65 km. The models suggest that 1-2 wt% H2O is released at the depths of NVT/SSEs in Jalisco-Colima, Guerrero, Cascadia, and Shikoku due to punctuated dehydration reactions within MORB, primarily through chlorite and/or lawsonite breakdown. These reactions produce sufficient in-situ fluid across a narrow P-T range to cause high pore fluid pressures at NVT/SSE depths. Dehydration of hydrated peridotite is minimal at these depths for most margins, and metapelite releases H2O (<1.5 wt%) gradually over a wide depth range compared to MORB. We posit that punctuated dehydration of oceanic crust provides the dominant source of fluids at the base of the seismogenic zone in these warm subduction zones, and up-dip migration of fluids from deeper in the subduction zone is not required." @default.
• W3091802355 created "2020-10-15" @default.
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• W3091802355 date "2020-12-01" @default.
• W3091802355 modified "2023-09-30" @default.
• W3091802355 title "Slab dehydration in warm subduction zones at depths of episodic slip and tremor" @default.
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• W3091802355 cites W1599932316 @default.
• W3091802355 cites W1695662870 @default.
• W3091802355 cites W1785387093 @default.
• W3091802355 cites W1847069267 @default.
• W3091802355 cites W1900036548 @default.
• W3091802355 cites W1965656370 @default.
• W3091802355 cites W1968228897 @default.
• W3091802355 cites W1970831581 @default.
• W3091802355 cites W1974393412 @default.
• W3091802355 cites W1974719076 @default.
• W3091802355 cites W1976215044 @default.
• W3091802355 cites W1976229064 @default.
• W3091802355 cites W1987046510 @default.
• W3091802355 cites W1996830300 @default.
• W3091802355 cites W1999125016 @default.
• W3091802355 cites W2001246549 @default.
• W3091802355 cites W2001538236 @default.
• W3091802355 cites W2006679467 @default.
• W3091802355 cites W2011706660 @default.
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• W3091802355 cites W2044626444 @default.
• W3091802355 cites W2049361833 @default.
• W3091802355 cites W2054747879 @default.
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• W3091802355 cites W2139085903 @default.
• W3091802355 cites W2145138436 @default.
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• W3091802355 doi "https://doi.org/10.1016/j.epsl.2020.116601" @default.
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