Presenters-0595: Difference between revisions
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|CSDMS meeting abstract presentation=Subduction zones are ever-evolving over a wide range of spatio-temporal scales, and there are a range of interactions between deep mantle flow and surface tectonics which are of relevance for processes from the megathrust cycle to the long-term evolution of the Earth. I review studies that seek to understand a number of the involved processes with a focus on the role of sediments and rheology for subduction rates and deep mantle structure, as well as the thermo-mechanical state of the mantle wedge. | |CSDMS meeting abstract presentation=Subduction zones are ever-evolving over a wide range of spatio-temporal scales, and there are a range of interactions between deep mantle flow and surface tectonics which are of relevance for processes from the megathrust cycle to the long-term evolution of the Earth. I review studies that seek to understand a number of the involved processes with a focus on the role of sediments and rheology for subduction rates and deep mantle structure, as well as the thermo-mechanical state of the mantle wedge. | ||
|CSDMS meeting youtube code=3SAzSCU8_TE | |CSDMS meeting youtube code=3SAzSCU8_TE | ||
|CSDMS meeting youtube views={{Youtube_3SAzSCU8_TE}} | |||
|CSDMS meeting participants=0 | |CSDMS meeting participants=0 | ||
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Revision as of 17:20, 28 May 2025
CSDMS 2023: Patterns and Processes Across Scales
Subduction dynamics and surface-deep mantle interactions
Abstract
Subduction zones are ever-evolving over a wide range of spatio-temporal scales, and there are a range of interactions between deep mantle flow and surface tectonics which are of relevance for processes from the megathrust cycle to the long-term evolution of the Earth. I review studies that seek to understand a number of the involved processes with a focus on the role of sediments and rheology for subduction rates and deep mantle structure, as well as the thermo-mechanical state of the mantle wedge.
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Of interest for:
