Discussion about the coupling relationship between the breakup of supercontinent and the large-scale manganese accumulation in China
DU Yuansheng1, YU Wenchao1, ZHOU Qi2, GUO Hua1, JIN Song3, LIU Zhichen4, HUANG Heng5, LIU Hai6, WANG Ping7, QI Liang8, XU Yuan1, XU Lingtong1, WANG Yuhang1, WANG Hanwen1
1 China University of Geosciences(Wuhan),Wuhan 430074,China; 2 Innovation Center of Ore Resources Exploration Technology in the Region of Bedrock,Ministry of Natural Resources of China,Guiyang 550081,China; 3 Geological Survey Institute of Hebei Province,Shijiazhuang 050081,sChina; 4 Geological Brigade 102 of Guizhou Province,Guizhou Zunyi 563003,China; 5 Geological Survey Institute of Guangxi Zhuang Autonomous Region,Nanning 530015,China; 6 Hubei Institute of Metallurgical Geology,Hubei Yichang 443000,China; 7 Henan Polytechnic University,Henan Jiaozuo 454000,China; 8 Chengdu University of Technology,Chengdu 610059,China
Abstract Sedimentary Mn carbonate deposits in China are accumulated in a large time scale and widely distributed. The metallogenic peaks are Mesoproterozoic Jixianian,Neoproterozoic Nanhuan and Sinian,Early Paleozoic Cambrian and Ordovician,Late Paleozoic Devonian,Carboniferous and Permian,and Mesozoic Triassic. Sedimentary Mn carbonate deposits are mainly distributed in stretching rift basin,including the Mesoproterozoic Yan-Liao Aulacogen in North China,the Nanhuan-Ordovician Nanhua Rift Basin,the Nanhuan intracontinental rift in northern Yangtze Block,the Sinian-Cambrian continental margin rift in northern Yangtze Block,Late Paleozoic-Triassic Youjiang Basin and the Xiang-Gui Aulacogen,the intracontinental trough in the western Yangtze Block(Shuicheng-Zunyi)and the trough in northwestern Yangtze Block. The source of the Mn carbonate deposit mainly comes from the deep hydrothermal fluid,which are then deposited in the shallow rift environment of suboxic deep water. The rift-type basins were formed during the breakup periods of the Columbia Supercontinent,the Rodinia Supercontinent and the Gondwana continent. There is an obvious coupling relationship between formations of the sedimentary Mn deposits and the breakup of supercontinents.
Fund:National Natural Science Foundation of China(No. U1812402)
About author: DU Yuansheng,born in 1958,is a professor and Ph.D. supervisor of China University of Geosciences(Wuhan). He is mainly engaged in the researches of sedimentology and geology of orogenic belt. E-mail: duyuansheng126@126.com.
Cite this article:
DU Yuansheng,YU Wenchao,ZHOU Qi et al. Discussion about the coupling relationship between the breakup of supercontinent and the large-scale manganese accumulation in China[J]. JOPC, 2023, 25(6): 1211-1234.
DU Yuansheng,YU Wenchao,ZHOU Qi et al. Discussion about the coupling relationship between the breakup of supercontinent and the large-scale manganese accumulation in China[J]. JOPC, 2023, 25(6): 1211-1234.
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