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- W2351043495 abstract "The Shuangxiwu Group and Shuangqiaoshan Group represent Precambrian basement strata of the Zhejiang-Jiangxi section of the Jiangnan Proterozoic Island Arc Zone. The Zhejiang-Jiangxi section of the Proterozoic Island Arc Zone can be classified based upon the differences in the rock formation of the basement strata and the distribution of ophiolites and collision granitoids along the Northeastern Jiangxi Fault belt. The two terranes are the Huaiyu tertrane and the Jiulin terrane. The Huaiyu terrane volcanic rocks predonmiate in the basement strata of 1. 0—1.3 Ga as the most important period for crustal formation whereas basement strata of the Jiulin terrane are characterized by turbidity flysch sediments as the terrare underwent crustal accretion during 1. 4—1.6 Ga. About 0. 6 Ga ago, the Jiulin and Huaiyu terranes collied with each other. Cathysia subsequently came into collision with the Jiangnan Proterozoic Island are Zone. Collisions terminated at about 0. 8 Ga with the subsequent deposition of Sinian cover." @default.
- W2351043495 created "2016-06-24" @default.
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- W2351043495 date "1993-01-01" @default.
- W2351043495 modified "2023-09-26" @default.
- W2351043495 title "CRUSTAL BASEMENT EVOLUTION OF THE ZHEJIANG - JIANGXI PORTION OF THE JIANGNAN PROTEROZOIC ISLAND ARC ZONE" @default.
- W2351043495 hasPublicationYear "1993" @default.
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