T33B:
Linking Surface and Upper Crustal Kinematics to Deeper Crust and Mantle Flow in Collisions I Posters
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T33B:
Linking Surface and Upper Crustal Kinematics to Deeper Crust and Mantle Flow in Collisions I Posters
Linking Surface and Upper Crustal Kinematics to Deeper Crust and Mantle Flow in Collisions I Posters
You can still search the program to see your colleague�s abstract submissions as well as the sessions submitted for the 2016 Fall Meeting. The final program will be released in early October.
Session ID#: 12954
Session Description:
Structural, chronological, geomorphic and geodetic studies of near surface kinematics in active orogens show a range of behaviors, including fold–thrust belts, footwall duplexing, major strike-slip shear, plateaus, extensional collapse of unsupported topography, and upwards extrusion of material from the deeper crust.
The extent to which the colliding lithospheres underneath force or follow these patterns is not well understood. In active orogens, flow at deeper levels must be inferred from geophysical datasets. The internal regions of ancient orogens reveal deeper patterns of deformation and metamorphism, but how these linked to surface movements is difficult to interpret. Numerical simulations are often used to test limiting cases.
We invite contributions from any discipline that explores how flow is coupled both vertically and laterally in the lithosphere during orogeny. Participants are encouraged to consider how their work illuminates connections between kinematics and mass transfer from the deepest to the shallowest levels of collisions.
The extent to which the colliding lithospheres underneath force or follow these patterns is not well understood. In active orogens, flow at deeper levels must be inferred from geophysical datasets. The internal regions of ancient orogens reveal deeper patterns of deformation and metamorphism, but how these linked to surface movements is difficult to interpret. Numerical simulations are often used to test limiting cases.
We invite contributions from any discipline that explores how flow is coupled both vertically and laterally in the lithosphere during orogeny. Participants are encouraged to consider how their work illuminates connections between kinematics and mass transfer from the deepest to the shallowest levels of collisions.
Primary Convener: David J Young, Ohio State University, Columbus, OH, United States
Conveners: Alison R Duvall, University of Washington, Earth and Space Sciences, Seattle, United States and Rebecca O Bendick, University of Montana, Geosciences, Missoula, MT, United States
Chairs: Alison R Duvall, University of Washington, Earth and Space Sciences, Seattle, United States, Rebecca O Bendick, University of Montana, Geosciences, Missoula, MT, United States and David J Young, Ohio State University, Columbus, OH, United States
OSPA Liaison: David J Young, Ohio State University, Columbus, OH, United States
Cross-Listed:
- EP - Earth and Planetary Surface Processes
- G - Geodesy
- S - Seismology
- V - Volcanology, Geochemistry and Petrology
Index Terms:
0905 Continental structures [EXPLORATION GEOPHYSICS]
1209 Tectonic deformation [GEODESY AND GRAVITY]
8011 Kinematics of crustal and mantle deformation [STRUCTURAL GEOLOGY]
8110 Continental tectonics: general [TECTONOPHYSICS]
Abstracts Submitted to this Session:
See more of: Tectonophysics
