Thermal evolution and dynamic mechanism of the Sichuan Basin during the Early Permian-Middle Triassic

查看全文 作　　者：HE [1]LiJuan;XU [2]HeHua;WANG [1]JiYang

机构地区：[1]State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;[2]CAS Key Laboratory of the Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China

出　　处：《Science China Earth Sciences》索引2011年第54卷第12期,共7页

基　　金：supported by Sinopec Marine Forward-looking Projects (Grant No. YPH08101) 摘　　要：The Sichuan Basin, located in the western margin of Yangtze Plate, is one of the important oil-gas-bearing basins in China. During the Early Permian-Middle Triassic, the Sichuan Basin experienced regional lithospheric extension and Emeishan basalt activities, both of which influenced the basin development and thermal evolution. Here we simulated the thermal effects of lithospheric extension and the Emeishan mantle plume based on different geodynamical models. Modeling results indicated that the lithospheric temperature together with the basement heat flow was generally increasing with time due to extension. As the stretching factor was relatively small, the thinning of lithosphere, and consequently the thermal disturbance, was not great. The lithospheric extension yielded about 20% increase of the basement heat flow, with maximum value of 60?62 mW m?2 in the Early Triassic. Mantle plume model shows that the thermal evolution of the inner zone above the plume head was influenced greatly by plume activity. But the outer zone and its outside area where the Sichuan Basin is located were affected only slightly. The basalts that had erupted in the southwestern basin might disturb the basin temperature significantly, although shortly and locally. Generally, the thermal history of the Sichuan basin during the Early Permian-Middle Triassic was controlled by the lithospheric extension, but locally it superimposed thermal effects of basalt activities in its southwestern area. 关键词：四川盆地早二叠世中三叠世热演化峨眉山玄武岩岩石圈伸展峨眉山地幔柱地球动力学模型

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Thermal evolution and dynamic mechanism of the Sichuan Basin during the Early Permian-Middle Triassic

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