T24A:
Deep Structures of the Eastern Tethyan Orogenic Belt and Related Geodynamics Processes I
T24A:
Deep Structures of the Eastern Tethyan Orogenic Belt and Related Geodynamics Processes I
Deep Structures of the Eastern Tethyan Orogenic Belt and Related Geodynamics Processes I
Submit an Abstract to this Session
Session ID#: 57125
Session Description:
The eastern Tethyan orogenic belt forms an active ~5000 km long continental collision/subduction belt, ranging from the Iranian plateau in the west to the Burma subduction zone in the east. The primary sources driving its formation are the collisions of India and Arabia with the southern margin of Asia which initiated during the Cenozoic and produced the Zagros and Himalayan orogenic belts, the Iranian and Tibetan plateaus, and also the Makran and Burma subduction zones. The crustal and upper mantle structures of this belt can provide unique constrains to understand the continental collision and subduction/collision transition processes. Numerous geophysical observations conducted in recent years across these orogenic systems allow in-depth exploration of the deep structures and related geodynamic processes. This session invites contributions to advance our understanding of the continental convergence in the Zagros-Pamir-Himalaya-Tibet-Burma belt from multiple geophysical disciplines, including, but not limited to, seismology, gravity, magnetotelluric, and numerical modeling.
Primary Convener: Xiaofeng Liang, Institute of Geology and Geophysics, Chinese Academy of Sciences, State Key Laboratory of Lithospheric Evolution, Beijing, China
Conveners: Sofia-Katerina Kufner, Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Potsdam, Germany, Xiaohui Yuan, Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany and Shunping Pei, Institute of Tibetan Plateau Research,Chinese Academy of Sciences, Beijing, China
Primary Liaison: Xiaofeng Liang, Institute of Geology and Geophysics, Chinese Academy of Sciences, State Key Laboratory of Lithospheric Evolution, Beijing, China
Chairs: Sofia-Katerina Kufner, Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Potsdam, Germany, Shunping Pei, Institute of Tibetan Plateau Research,Chinese Academy of Sciences, Beijing, China and Xiaofeng Liang, Institute of Geology and Geophysics, CAS, Beijing, China
OSPA Liaison: Sofia-Katerina Kufner, Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Potsdam, Germany
Index Terms:
0925 Magnetic and electrical methods [EXPLORATION GEOPHYSICS]
7218 Lithosphere [SEISMOLOGY]
8104 Continental margins: convergent [TECTONOPHYSICS]
8123 Dynamics: seismotectonics [TECTONOPHYSICS]
Abstracts Submitted to this Session:
Recent research progresses on the deep structure and evolution of the Iranian Plateau (Invited) (347171)
See more of: Tectonophysics
