supported by the National Natural Science Foundation of China (Grant Nos.42025201,92155001,41802062,41888101);the Second Tibetan Plateau Scientific Expedition and Research Program (Grant No.2019QZKK0801)。
The evolution and final closure of the Neo-Tethys Ocean are one of the most important geological events that have occurred on Earth since the Mesozoic.However,the evolution of the Neo-Tethys is not well constrained,in...
the National Natural Science Foundation of China(Grant Nos.41572180 and 41630207).
The subduction channel is defined as a relatively thin and weak zone with coherent kinematics between the descending and overriding plates during subduction.The materials in the channel,showing the characteristics of ...
Supported by the National Natural Science Foundation of China (Grant Nos. 40234041 and 40272042)
The geodynamic setting of the Bikou volcanic group is a critical question to trace the Precambrain tectonic framework and evolution for the Yangtze plate. This study has suggested that the Bikou volcanic group is comp...
New paleontological evidence suggests that the composition of the matrix and slices from the middle and the south of the Eastern Kunlun Mélange Belt is very complex, ranging from Proterozoic to Mesozoic in geological...
This work was jointly supported by the Foundation for University Key Teacher of the Ministry of Education ; the National Natural Science Foundation of China (Grant No.49732080) ; the Special Science Foundation of Shaanxi Province.
Detailed studies indicate that Kangxian-Pipasi-Nanping tectonic zone is a complicated mélange zone which includes many tectonic slabs of different origins. Ophiolite (MORB-type basalt), oceanic island tholeiite and a...