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The relationship of the formation and evolution of Mesozoic Chuxiong Basin to Ailaoshan orogenic belt in central Yunnan, China; exemplified by regional geological integrated section from Xishelu of Chuxiong to Bichengzhen of Lufeng



The relationship of the formation and evolution of Mesozoic Chuxiong Basin to Ailaoshan orogenic belt in central Yunnan, China; exemplified by regional geological integrated section from Xishelu of Chuxiong to Bichengzhen of Lufeng



Diqiu Xuebao = Acta Geoscientia Sinica 23(2): 129-134



It is shown that the formation and evolution of Chuxiong Basin are related to Ailaoshan orogenic belt in Late Triassic. It is a backland basin of Ailaoshan orogenic belt instead of a foreland basin as some geologists have considered. Although it developed at the same time as the foreland basins that lie in the west of Ailaoshan orogenic belt, their rock assemblages and sedimentary facies are quite different.

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