Deflection rheoevolution of lithosphere under subduction |
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| Authors: | Yuying Han Weixiang Wang |
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| Institution: | (1) College of Earth Science, China University of Geosciences, 430074 Wuhan, China;(2) Department of Geology, China University of Geosciences, 100083 Beijing, China;(3) Department of Geology, China University of Geosciences, 100083 Beijing, China |
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| Abstract: | Along the continental margin, the tectonic system consisting of trench, island are, back are basin and outer rise is often
known as a convergent transitional belt between the oceanic lithosphere and the continental lithosphere. The occurrence, development
and activity of trench and outer rise bear closely on the underthrusting process of the oceanic lithosphere. A generalized
analytical theory of deflection rheoevolution of lithosphere under subduction is established, and solutions with universal
significance have been obtained.
Project supported by the Laboratory of Lithosphere Tectonics and Its Dynamics of Ministry of Geology and Mineral Resources
of China. |
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| Keywords: | lithosphere subduction rheoevolution outer rise geodynamics |
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