supported by the Basic Scientific Fund for National Public Research Institutes of China(Grant No.2023S02);the National Natural Science Foundation of China(Grant Nos.42076076&42376075);the Taishan Scholar Program of Shandong Province。
Oceanic intraplate volcanoes with linear age progressions are usually accepted to be derived from melting of an upwelling mantle plume.Several seamount groups in NW Pacific,however,show complex age-distance relationsh...
supported by the National Natural Science Foundation of China (Grant Nos. 41630207, 41572180);the China Geological Survey Project (Grant No. 12120115027001)
In the northern West Qinling orogen(WQO), granulite-facies metamorphic rocks are recognized within the Qinling Complex. These rocks are composed of amphibole-bearing two-pyroxene granulite and garnet-sillimanite gneis...
supported by the National Natural Science Foundation of China (Grant No. 90814006);111 Project (Grant No. B07011)
Various extensional structures,e.g.,half grabens,detachment faults,and metamorphic core complexes,were formed in the Liaodong Peninsula.There are two metamorphic core complexes (mcc's) in the western part of the Penin...
supported by National Natural Science Foundation of China (Grant Nos.40634022,40972132);State Key Laboratory for Mineral Deposits Research of Nanjing University (Grant No.2008-I-01)
Using the U-Pb LA-ICP-MS analysis technique we analyzed geochronological features of detrital zircons from Devonian and Ordovician coarse sandstone in southern Jiangxi Province,northern Cathaysia Block.Abundant ancien...
supported by National Basic Research Program of China (Grant No.2009CB825003);National Natural Science Foundation of China (Grant No.40972128);China Geological Survey "Comprehensive Research of Precambrian Geology and Paleozoic Tectono-paleogeography in Qing-hai-Tibet Plateau"
The CL images,LA-ICP-MS in situ trace elements analysis,and U-Pb dating for zircons indicate that the metamorphic ages of the sillimanite-garnet-biotite gneiss and the garnet-amphibole gneiss from eastern Taxkorgan of...
Supported by National Basic Research Program of China (Grant No. 2006CB403504)
Zircon U-Pb results of basalt from the Dashizhai Town in Inner Mongolia, NE China, shows that the basaltic lava was erupted at 439±3 Ma, much older than the "Permian basalts" as previously thought. These rocks show a...
the National Natural Science Foundation of China (Grant No. 40621002);the Foundation of Geological Survey of China (Grant No. 1212010610103);MOE Innovative Research Team Program (Grant No. IRT0546)
Geological mapping data (1:250000) in the Qinghai-Tibet Plateau and its adjacent regions reveal the sediment sequences, distribution and tectonic evolution of the 92 Tertiary remnant basins. Southern Tibet and the Yec...
the National Natural Science Foundation of China (GrantNo.40334037);the Fund for Creative Research Groups (Grant No.40521001)
The Tiefosi granitic pluton is located 5 km northwest of Xinyang City, northern Dabie Orogen, and was emplaced in the Proterozoic Qinling Group. SHRIMP zircon U-Pb dating suggests its crystallization at 436 ± 11 Ma. ...
This work was supported by the National Natural Science Foundation of China (Grant No. 49572100); the Foundation of the Education Ministry of China for University Key Teachers.
Regional architecture of geochronology and differential cooling pattern show that the Dabie orogen underwent a thermal doming extension during 140-85 Ma. This extension resulted in widespread re-melting of the Dabie b...
The khondalite series, which are characterized by aluminum-rich gneisses (schists) consisting of sillimanite-garnet-biotite-monzonite gneiss, garnet-biotite-monzonite gneiss, graphite-sillimanite-biotite schist, and g...