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《Earth Science Frontiers》 2000-04
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TYPES AND TECTONIC EVOLUTION OF JUNGER BASIN

CAI Zhong xian 1, CHEN Fa jing 2, JIA Zhen yuan 2(1 University of Petroleum, Beijing 102200,China; 2 China University of Geosciences, Beijing 100083, China)  
Junggar basin is a large continental interior basin in western China, which has been developing since Early Permian Controversy focuses on the type of basin in Early Permian and its origin Also the attributions of the basin from Triassic to Early Tertiary is unknown Evidences about basin fill architecture, tectonic subsidence, geo thermal histories, petrological and geochemical characteristics of Early Permo carboniferous volcanic rocks can provide the following new recognition (1) The basin was initially rifted in Early Permian followed by thermal cooling subsidence during Late Permian, thence went through the cratonic basin stage from Triassic to Paleogene, and finally through the foreland basin developing (2)A large number of calc alkaline suite volcanic rocks erupted in early Permo Carboniferous accompanied by type A granites intrusion suggest that the rift in Early Permian was related to postorogenic extension collapse Furthermore soft collision was a tectonic background for postorogenic extension collapse during Paleozoic in Northern Xinjiang (3) The driving mechanism of postorogenic extension collapse was a mantle thermal convection
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