Presenters-0680: Difference between revisions
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|CSDMS meeting email address=John.naliboff@nmt.edu | |CSDMS meeting email address=John.naliboff@nmt.edu | ||
|CSDMS meeting title presentation=Feedbacks between coupled surface processes and lithospheric deformation during multiphase continental rifting | |CSDMS meeting title presentation=Feedbacks between coupled surface processes and lithospheric deformation during multiphase continental rifting | ||
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{{Presenters coauthors | |||
|CSDMS meeting first name co1=Liang | |||
|CSDMS meeting last name co1=Xue | |||
|CSDMS meeting institute co1=Syracuse University | |||
|CSDMS meeting country co1=United States | |||
|CSDMS meeting state co1=New York | |||
|CSDMS meeting email address co1=lxue07@syr.edu | |||
}} | }} | ||
{{Presenters presentation | {{Presenters presentation | ||
Revision as of 07:26, 24 January 2025
CSDMS 2025: Exploring Earth's Surface with Models, Data & AI
Feedbacks between coupled surface processes and lithospheric deformation during multiphase continental rifting
Abstract
Recent advances in coupled simulation of solid Earth deformation and landscape evolution have provided new insights into the feedbacks between tectonic and surface processes acting across vastly different spatiotemporal scales. Recent work across the geodynamics community has highlighted the significant role of erosion and sedimentation in the lithospheric deformation across different tectonics regimes. For example, multiple studies have illustrated the impact of surface processes on the timing, style, and progression of continental rifting, which in turn shapes the evolution of landscapes. This presentation aims to showcase recent advancements from community-driven efforts and present new results utilizing the Advanced Solver for Planetary Evolution, Convection, and Tectonics (ASPECT) and Fastscape that examine complex styles of faulting, landscape, and basin evolution during multiphase rifting. Focused applications will include the role of structural inheritance on rift initiation to continental breakup across a wide range of rifting conditions. The results of such coupled simulation have broad implications for understanding the factors governing the stability and longevity of rift basins, the development of natural resources, and potential responses of tectonic systems to surface processes under varying hydroclimatic conditions.
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