supported by the National Natural Science Foundation of China(Nos.U22B6002,42422402,41902202 and 42276222);the SINOPEC Key Laboratory of Geophysics(No.FW0399-0029);the Second Tibetan Plateau Scientific Expedition and Research(No.2019QZKK00708);the Development Fund of South China Sea Institute of Oceanology of the Chinese Academy of Sciences(No.SCSIO202207);the Special Fund of the Institute of Geophysics,China Earthquake Administration(No.DQJB22B23)。
The boundary between cratonic and orogenic lithospheres is a significant seismogenic zones marked by intense lithospheric deformation.The Sichuan Craton(SCC),as a key tectonic block bordering eastern Tibetan Plateau,r...
supported by the project of China Geological Survey(Grant No.DD20190438)。
The timing and mechanisms of lithospheric thinning and destruction of the North China Craton(NCC)remain controversial,and the overall geodynamics of the process are poorly understood.This paper documents Late Triassic...
funded by the National Key Research and Development Program of China(2016YFC0601005);the Geological Survey of China(DD20190370,DD20190811,cdcgs2018001);the National Science Foundation of China(41772107,41772016);the 13th Five-year Plan of the Ministry of Science and Technology of China(2016ZX05034-002-003)。
The continent of China developed through the coalescence of three major cratons(North China, Tarim and Yangtze) and continental micro-blocks through the processes of oceanic crust disappearance and acceretionary-colli...
supported by the National Natural Science Foundation of China (Grant No. 41473015);a research grant from the Institute of Crustal Dynamics, CEA (ZDJ2014-02; ZDJ2017-05);the Tutor Foundation of the China University of Geosciences (Beijing) (Grant No. 53200859400);the China Geological Survey Projects (Grant Nos. 12120114041401 and 12120113015700)
This study describes a previously unidentified Neoproterozoic mafic dyke emplaced in the northern flank of the Langshan Tectonic Belt. This dyke intruded into the micaquartz schist of the Zhaertaishan Group, and yield...
Financial supports for this study were jointly supported by the National Natural Science Foundation of China (Grant Nos.41421002 and 41602109);most special fund from the State Key Laboratory of Continental Dynamics, Northwest University, Shaanxi Postdoctoral Science Foundation, National Science and Technology Special Grant (No. 2016ZX05006-007);China Geological SurveyGrant (No. DD20189614)
The Helanshan tectonic belt is located to the west of the Ordos Basin, and separates the Alxa(or Yinshan)Massif to the west from the Ordos block to the east. Triassic sedimentation in the Helanshan tectonic belt recor...
the National Natural Science Foundation of China (Grant No. 41272066);the National Science and Technology Support Program (Grant No. 2012BAK19B04-01);the Yangtze River Scholars and Innovation Team Development Plan (Grant No. IRT13075)
More than 80 layers of seismites were recognized from the Early Cretaceous Dasheng Group in the Mazhan and Tancheng graben basins in the Tanlu Fault Zone, eastern China. The responsible seismic events took place about...
The Amazonian craton major accretionary and collisional processes may be correlated to supercontinent assemblies developed at several times in the Earth history. Based on geologic, structural and paleomagnetic evidenc...