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- W2348127444 abstract "The Dabie shan orogen represents a contractional belt of intracontinent in Mesozoic Era and its fundamental tectonic system is characterized by a tectonic wedge towards south, which consists of a overthrust nappe structrue. The propagation style of the four main overthrust faults, which constitute overthrust system, is backward compared to the root zone from south to north. For the sake of the structural deformation of the rock system of the basement and sedimentary covers the large scale thin skinned structure formed, and the shortening of crust amounts to 48 6 percent. The overthrust nappe tectonic system in the Dabieshan orogenic belt accomplished from later Lower Jurassic to Early Cretaceous (J 3 1-K 1)." @default.
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- W2348127444 date "2002-01-01" @default.
- W2348127444 modified "2023-09-25" @default.
- W2348127444 title "MESOZOIC OVERTHRUST-NAPPE TECTONIC SYSTEM IN THE DABIESHAN OROGENIC BELT" @default.
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