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《Acta Geologica Sinica》 1995-03
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THE UPLIFT OF THE LONGMENSHAN THRUST BELT AND SUBSIDENCE OF THE WESTERN SICHUAN FORELAND BASIN

Liu Shugen, Luo Zhili, Dai Solan,(Chengdu institute of Technology, Chengdu, Sichuan, China)Dennis Arne(Dalhousie University, Canada)and C. J. L. Wilson(Melbourne University, Ausiralia)  
Through the measurement and computer modelling of the apatite fission track data and vitrinite reflectance, the uplift history of the Longmenshan thrust belt and uplift (subsidence) history of the Western Sichuan foreland basin have been studied in details. The Songpan-Garze fold belt has been uplifted at least 3-4km since 10Ma B. P., with an uplift rate of at least 0.3-0.4mm/a. The Logmenshan thrust nappe belt has been uplifted 5-6km at least since 10Ma B. P., with an uplift rate of more than 0.5-0.6mm/a. The Longmenshan foreland detachment belt has been uplifted 1-2km since 60 Ma B. P., with an uplift rate of 0.016-0.032mm/a. The Western Sichuan foreland basin has been uplifted 1.7-3km since 60Ma B.P., with an uplift rate of 0.028-0.05mm/a. The uplift rate on the western side of the Beichuan-Yingxiu-Xiaguanzi fault is 40 times as much as that on its eastern side since 10Ma B. P. The palaeo-temperature gradient was 25℃/km in the Western Sichuan foreland basin.
【Fund】: 中国自然科学基金(编号 49070140)
【CateGory Index】: P544.4
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