Subduction characteristics of the ordovician erlangping back-arc basin in the east qinling mountains, china: implications for the tectonic evolution of the northern margin of the proto-tethys ocean
Author:
Affiliation:
1. School of Resources and Environmental Engineering, Hefei University of Technology, Hefei, China
2. School of Electronic Science and Engineering, Nanjing University, Nanjing, China
Funder
National Natural Science Foundation of China
Publisher
Informa UK Limited
Subject
Geology
Link
https://www.tandfonline.com/doi/pdf/10.1080/00206814.2021.1891580
Reference96 articles.
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2. Alleghanian tectono-thermal evolution of the dextral transcurrent Hylas zone, Virginia Piedmont, U.S.A.
3. Cheng, S.X., 2014, Tectonic Evolution and Assembly of the east segment of northern boundary of the Proto-Tethys Ocean (Master’s thesis). Ocean University of China.
4. Orientation analysis of localized shear deformation in quartz fibres at the brittle–ductile transition
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2. Structural Geology and Chronology of Shear Zones along the Shangdan Suture in Qinling Orogenic Belt, China: Implications for Late Mesozoic Intra-Continental Deformation of East Asia;Journal of Earth Science;2024-04
3. Early Paleozoic arc-accretion in the northern branch of the Proto-Tethys Ocean: New insights from detrital zircon U Pb ages and geochemistry of paraschists from the Kuanping Complex, North Qinling Orogenic Belt, China;Lithos;2021-11
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