T11B:
Observations and Models of Multiphase Deformation in Rifts and Rifted Margins I
T11B:
Observations and Models of Multiphase Deformation in Rifts and Rifted Margins I
Observations and Models of Multiphase Deformation in Rifts and Rifted Margins I
Submit an Abstract to this Session
Session ID#: 57083
Session Description:
Observations from rifts and rifted margins suggest continental extension commonly involves multiple phases of deformation with distinct structural, sedimentary and magmatic characteristics. In many rifts, deformation evolves both as a function of time and location, and rift architecture may reflect the influence of structural inheritance, evolution of the lithosphere’s thermal-mechanical profile, feedbacks between surface process and lithospheric deformation or large-scale changes in plate driving forces. Here, we solicit presentations that examine the long-term evolution of continental rift systems through field, geophysical and numerical investigations. In particular, we encourage submissions that focus on the processes driving changes in deformation style and use large 3-D observational or numerical data sets to characterize lithospheric deformation.
Primary Convener: John Naliboff, University of California Davis, Davis, CA, United States; University of California, Davis, Computational Infrastructure for Geodynamics (CIG), Earth and Planetary Sciences Department, Davis, CA, United States
Conveners: Rebecca E Bell, Imperial College London, Department of Earth Science and Engineering, London, United Kingdom, Jolante van Wijk, New Mexico Institute of Mining and Technology, Earth & Environmental Science, Socorro, United States and Scott E K Bennett, USGS, Geology Minerals Energy and Geophysics Science Center, Menlo Park, CA, United States
Primary Liaison: John Naliboff, University of California, Davis, Computational Infrastructure for Geodynamics (CIG), Earth and Planetary Sciences Department, Davis, CA, United States; University of California Davis, Davis, CA, United States
Chairs: Jolante van Wijk, New Mexico Institute of Mining and Technology, Earth & Environmental Science, Socorro, United States and John Naliboff, University of California, Davis, Computational Infrastructure for Geodynamics (CIG), Earth and Planetary Sciences Department, Davis, CA, United States; University of California Davis, Davis, CA, United States
OSPA Liaison: John Naliboff, University of California, Davis, Computational Infrastructure for Geodynamics (CIG), Earth and Planetary Sciences Department, Davis, CA, United States; University of California Davis, Davis, CA, United States
Index Terms:
8105 Continental margins: divergent [TECTONOPHYSICS]
8109 Continental tectonics: extensional [TECTONOPHYSICS]
8120 Dynamics of lithosphere and mantle: general [TECTONOPHYSICS]
8159 Rheology: crust and lithosphere [TECTONOPHYSICS]
Abstracts Submitted to this Session:
Spatial and Temporal Variations in Crustal Kinematics Across the Lake Tanganyika Rift, East Africa. (375936)
See more of: Tectonophysics
