Metamorphic P-T conditions and ages of garnet-biotite schists in the Dahongshan Group from the southwestern Yangtze BlockOAEI
The Dahongshan Group,situated at the southwestern margin of the Yangtze Block,represents a geological unit characterized by relatively high-grade metamorphism in the region.This paper investigates the garnet-biotite schist…查看全部>>
Jun-xiao Ma;Guang-shu Yang;Yong-feng Yan;Xiao-Fei Xu;Yun-hua Ren;Hui Zhao;Xiao-jun Zheng;Yuan Qin
Faculty of Land Resources Engineering,Kunming University of Science and Technology,Kunming 650093,ChinaFaculty of Land Resources Engineering,Kunming University of Science and Technology,Kunming 650093,ChinaFaculty of Land Resources Engineering,Kunming University of Science and Technology,Kunming 650093,ChinaFaculty of Land Resources Engineering,Kunming University of Science and Technology,Kunming 650093,ChinaGeological Team 306 of Yunnan Non-Ferrous Metals Geological Bureau,Kunming 650217,ChinaFaculty of Land Resources Engineering,Kunming University of Science and Technology,Kunming 650093,ChinaFaculty of Land Resources Engineering,Kunming University of Science and Technology,Kunming 650093,China Yunnan Provincial Bureau of Non-Ferrous Geology,Kunming 650051,ChinaFaculty of Land Resources Engineering,Kunming University of Science and Technology,Kunming 650093,China
地质学
Southwestern Yangtze BlockDahongshan GroupPhase equilibrium modelingZircon U-Pb datingNeoproterozoic metamorphism
《Acta Geochimica》 2024 (4)
P.707-718,12
supported by the National Natural Science Foundation of China(Grant Nos.42162012,42072094)the Key Laboratory of Sanjiang Metallogeny and Resource Exploration and Utilization,Ministry of Natural Resources(Project No.ZRZYBSJSYS2022001).
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