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- W2371131486 abstract "The low degree of metamorphic rock units in South Anhui were formed by the assemblage of four tectonic units around the region.Before the early Meso-Proterozoic,it was ancient island arc around South Anhui.1000Ma ago,South China Block subducted along the Jiangshan-Shaoxing zone and made the island arc accret onto the Yangtze Block.900Ma,the spreading of back-arc basin took place along Qimen-Sanyangkeng.Around 850Ma,the cathysian Block collided with the Yangtze Block along the Jiangshan-Shaoxing zone,which marked the completion of subduction and accretion.The continental crust remelted to form the S-type granitoid intrusions,such as Xiuning,Xucun and Shexian intrusions.At about 780Ma,the gradual subduction of South China Sea led to the collision between South China and Yangtze blocks,and the final closing of Qimen-Sanyang sea,such as the Qimen-Sanyangkeng suture.This collision also induced the primary continental crust to remelt and then the magma emplaced within the plate to form the Lingshan,Lianhua and Baiji intrusions.Eventually it formed the volcanic rock nappe of Baiji Ridge,and marked the formation of tectonic framework in the South Anhui.The tectonic evolution not only resulted in the structural pattern of the district,but also controlled the distribution of regional mineral.The Jinning and Yangshan Periods are the main time of mineralization in South Anhui.The Mesozoic mineralization was resulted from the evolution of partly metamorphic basement aged in the Jinning.The mineral distribution in Mesozoic time still indicates that the pattern of basement can control the regional mineralization." @default.
- W2371131486 created "2016-06-24" @default.
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- W2371131486 date "2008-01-01" @default.
- W2371131486 modified "2023-09-25" @default.
- W2371131486 title "THE TECTONIC EVOLUTION OF LOWER-METAMORPHIC ROCKS AND THE DISTRIBUTION DISTRICT OF MINERAL IN SOUTH ANHUI" @default.
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