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- W2352487904 abstract "There exist the Jingpin intracontinent thrust nappe belt, foreland thrust nappe belt and foreland uplift belt in the Jinping area, Sichuan. Based on the characteristics of structural units in this area, this paper proposes that the Chapuzi Baze regional revival fault is the regional boundary fault, and points out the Yangtze paraplatform western edge is a thrust fold belt that turns into the continental passive edge in Sinian Triassic Period on the basis of the pre Sinian basement and involves collision orogenesis in Mesozoic Era." @default.
- W2352487904 created "2016-06-24" @default.
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- W2352487904 date "2003-01-01" @default.
- W2352487904 modified "2023-09-25" @default.
- W2352487904 title "FORMATION AND EVOLUTION OF MESOZOIC THRUST FOLD BELT IN JINPING AREA, SICHUAN" @default.
- W2352487904 hasPublicationYear "2003" @default.
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