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《Acta Sedimentologica Sinica》 2002-04
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Analysis of Tectonic Uplift and Heavy Minerals of Sediments on Jiuxi Basin in the Northern Margin of Tibetan Plateau since the Late Cenozoic

SONG Chun hui 1,2 SUN Shu rong 1 FANG Xiao min 1,2 SUN Dong 1 1(National Laboratory of Western China's Environmental Systems and College of Resources and Environment, Lanzhou University, Lanzhou 730000) 2(State Key Laboratory of Loess and Quaternary Geology and Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, Shaanxi 710075)  
Sediments in basins could record the ascending and descending difference of the earth crust. The sediments of the Late Cenozoic in the Jiuxi basin, located in the northern margin of the Tibetan plateau, have sensitively and completely recorded the uplifting process of northern plateau. The heavy minerals of sediments have the regulatory variety in the Laojunmiao section of Jiuxi basin since 13 MaBP; detailed study of the heavy mineral has revealed four heavy mineral stages of sedimentary evolution. they are: ①stable heavy mineral associations before 12.18 Ma BP , ②relatively stable heavy mineral associations between 12.18 and 8.26 Ma BP, ③unstable heavy mineral associations between 8.26 and 4.9 Ma BP, and ④the very unstable heavy mineral associations since 3.66 Ma BP. The associated mountain erosion and uplift are suggested having experienced three phases on the uplifting process of the northern Tibetan Plateau, that is, tectonic stable (13~ 8.26 Ma BP), gradual staggered uplift (8.26~4.96 Ma BP), and rapid intense intermittent mass uplift (3.66~0 Ma BP).
【Fund】: 国家教委重大项目 (0 0 - 0 5);; 国家重点基础研究发展规划 (G1 9980 4 0 80 9)资助
【CateGory Index】: P542
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