supported by the National Natural Science Foundation of China(Grant No.41903032);Science(Engineering)Research Project of Yunnan University(Grant No.2017YDQN08);Applied Basic Research Programs of Science and Technology Department of Yunnan Province(Grant No.2018FD009).
A comprehensive study of zircon U-Pb geochronology,in situ Hf isotopes,whole-rock major and trace element geochemistry,and Nd isotopes was carried out for two Early Jurassic two-mica granites(Longtang and Menglong)in ...
This study was financially supported by the Major Science and Technology Special Plan of Yunnan Province(Grant No.202202AG050006);the National Natural Science Foundation of China(Grant No.41603032);the Applied Basic Research Foundation of Yunnan Province(Grant No.2017FB075);the Yunnan Key Research and Development Program(Grant No.2015CB452601),and the China Geological Survey(Grant No.12120114064301).
The Changning-Menglian Belt represents the main Paleo-Tethyan Suture in the southeastern Tibetan Plateau,which divides Gondwana-and Eurasia-derived continental fragments from each other.The belt contains ultramafic-ma...
financially supported by the National Natural Science Foundation of China(Grant 91855206);National Key Research and Development Project of China(Grant 2016YFC0600310);the Foundation of Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources(No.J1901-18,J1901-23)。
The Jinghong mafic-ultramafic complex,exposed in the eastern margin of the Lancangjiang tectonic belt,is related to the subduction of the Paleo-Tethys Ocean.Its petrogenesis plays a key role in constraining the tecton...
funded by a grant from the National Key R&D Program of China(Grant No.2018YFC0604106 and 2016YFC0600305);the Program of the China Geological Survey(Grant No.DD20190053)。
The Jiangda–Deqen–Weixi continental margin arc(DWCA) developed along the base of the Changdu–Simao Block and was formed as a result of the subduction of the Jinsha River Ocean Slab and the subsequent collision. The...
supported by the National Natural Science Foundation of China(Grant Nos.91755103 and 41872240);the Ministry of Science and Technology of China(2016YFC0600304);the Chinese Geological Survey Project(Grant Nos.DD20190370 and DD20190060);the Institute of Geology of the Chinese Academy of Geological Sciences Research Fund(Grant Nos.J1705 and YYWF201704)
The Paleo-Tethys Ocean is usually interpreted as a Paleozoic ocean basin located between the Gondwana and Laurasia supercontinents. The Paleo-Tethyan orogenic record is well preserved in the Sanjiang area of SW China....
financially supported by the National Natural Science Foundation of China(grants No.41602105,41530966,41672106 and 41472086);China Postdoctoral Science Foundation(grant No.2016M590655);the fundamental Research Funds for the Central Universities,Ocean University of China
Objective The eastern extending range of the Paleo-Tethys Ocean in southwest China has always been focused and controversial. At the beginning of this century some scholars proposed that the Paleo-Tethys Branch Ocean...