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Fluid escape from subduction zones controlled by channel-forming reactive porosity
O. Plümper
*
, Timm John
*
, Y.Y. Podladchikov
, J.C. Vrijmoed
, M. Scambelluri
*
Corresponding author for this work
DES - Structural geology & Electron microscopy group
Research Programme in Earth Sciences Utrecht (DES / IVAU)
Freie Universität Berlin
University of Lausanne
Dipartimento di Scienze della Terra
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Keyphrases
Porosity
100%
Subduction Zone
100%
Dehydration Reaction
100%
Channel Shape
100%
Fluid Escape
100%
High Pressure
33%
Earth Surface
33%
Oceanic Lithosphere
33%
Subduction
33%
Fluid Pressure
33%
Subducting Plate
33%
Subducting Slab
33%
Fluid Flow
33%
Pressure Variation
33%
Channel Network
33%
Thermodynamic Modeling
33%
Serpentinite
33%
Intermediate Depth
33%
Channelization
33%
Chemical Heterogeneity
33%
Reactive Fluid
33%
Rock Physics Analysis
33%
Fluid Release
33%
Microsite
33%
Embrittlement
33%
Subduction Zone Seismicity
33%
Chemically Bound Water
33%
Porosity Generation
33%
Vein Network
33%
Flow Initiation
33%
Antigorite Dehydration
33%
Earth and Planetary Sciences
Subduction Zone
100%
Porosity
100%
Earth Surface
33%
Fluid Pressure
33%
Oceanic Lithosphere
33%
Fluid Flow
33%
Seismicity
33%
Serpentinite
33%
Antigorite
33%
Embrittlement
33%