T21B:
The Varied Roles of Aqueous Fluids near the Subduction Interface I
T21B:
The Varied Roles of Aqueous Fluids near the Subduction Interface I
The Varied Roles of Aqueous Fluids near the Subduction Interface I
Submit an Abstract to this Session
Session ID#: 57195
Session Description:
Along the subduction plate interface, water influences the rheological and geophysical properties as well as the rates and products of metamorphic reactions. Recent geologic and seismic studies demonstrate that strong feedbacks exist between the fluid-mediated chemical and petrologic evolution of the rock, deformation processes that control fault slip behavior, and geophysical signals we use to interpret physical conditions at depth. Fluid distribution and flux are thought to vary with depth and the permeability structure near the plate interface. These fluids are proposed to control episodic tremor-and-slip, dehydration-induced seismicity, serpentinization of the mantle wedge, overriding plate alteration, and the 4-D evolution in interface bulk-rock compositions, active deformation mechanisms, and rock strength. We invite contributions addressing the varied influence of aqueous fluids near the subduction interface from across the Earth science community including, but not limited to: experimental studies, geodynamics, petrology/geochemistry, structural geology, and geophysics.
Primary Convener: Cailey Brown Condit, Massachusetts Institute of Technology, Cambridge, MA, United States
Conveners: Dr. Besim Dragovic, Ph.D., Boise State University, Department of Geosciences, Boise, ID, United States, Jonathan R Delph, Purdue University, Earth, Atmospheric, and Planetary Sciences, West Lafayette, IN, United States and Melodie E French, Rice University, Earth, Environmental and Planetary Sciences, Houston, TX, United States
Primary Liaison: Cailey Brown Condit, Massachusetts Institute of Technology, Cambridge, MA, United States
Chairs: Jonathan R Delph, Purdue University, Earth, Atmospheric, and Planetary Sciences, West Lafayette, IN, United States and Dr. Besim Dragovic, Ph.D., Boise State University, Department of Geosciences, Boise, ID, United States
OSPA Liaison: Cailey Brown Condit, Massachusetts Institute of Technology, Cambridge, MA, United States
Co-Organized
with:
Tectonophysics, and Volcanology, Geochemistry and Petrology
Tectonophysics, and Volcanology, Geochemistry and Petrology
Cross-Listed:
- MR - Mineral and Rock Physics
- S - Seismology
- V - Volcanology, Geochemistry and Petrology
Proposed Co-Organized Session with:
- MR - Mineral and Rock Physics
- V - Volcanology, Geochemistry and Petrology
Index Terms:
1031 Subduction zone processes [GEOCHEMISTRY]
7240 Subduction zones [SEISMOLOGY]
8045 Role of fluids [STRUCTURAL GEOLOGY]
8170 Subduction zone processes [TECTONOPHYSICS]
Abstracts Submitted to this Session:
Mechanism of fluid flow near the plate interface: the importance of a thin, low viscosity layer (387696)
See more of: Tectonophysics
