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《ACTA GEOLOGICA SICHUAN》 1996-03
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A PRIMARY DISCUSSION ON THE OROGENIC MODEL FOR INNER CONTINENTAL OROGENIC BELTS──On the example of Longmenshan orogenic belt

Lin Maobing (Dept. of Geology, Chengdu institute of Technology)  
Longmenshan orogenic belt is a typical example of inner continental orogenic belts. It has a long evolution history. During the Precambrian, it represented an active continental margin with stong magmatism and metamorphism as well as tectonic mixing. In the Paleozoic, it was in a condition of platform with tremendous platform facies sediments predominated by carbonate rock.In the early Mesozoic, it began to enter into inner continental orogenic stage and changed from fold orogeny in the early stage to nappe orogeny in the late stage. The two orogenies were companied by two types of foreland basins with different sediments. The last regional tectonics recorded and preserved more or less features of different inner continental orogenies. Of course,the last nappe orogeny had the heaviest and deepest influence. Dynamics of inner continental orogeny is closely related to the general environment of plate movement.
【CateGory Index】: P542
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