【作者】 颜茂都； Rob Van der Voo； 方小敏； 宋春晖；

【Author】 Maodu Yan~1 Rob Van der Voo~2 Xiaomin Fang~(1,3) Chunhui Song~1 1.Key Laboratory of Continental Collision and Plateau Uplift,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100085; 2.Department of Geological Sciences,University of Michigan, 1100 N University Ave,Ann Arbor,MI 48109-1005,USA; 3.National Laboratory of Western China’s Environmental Systems,Ministry of Education of China & College of Resources and Environment,Lanzhou University,Gansu 730000

【机构】 Key Laboratory of Continental Collision and Plateau Uplift,Institute of Tibetan Plateau Research,Chinese Academy of Sciences； Department of Geological Sciences,University of Michigan,1100 N University Ave,Ann Arbor,MI 48109-1005,USA； National Laboratory of Western China’s Environmental Systems,Ministry of Education of China & College of Resources and Environment,Lanzhou University；

【摘要】 <正>As products of nearby relief,sediments in tectonically active basins usually reflect the related controls of erosional,depositional,and structural processes.Studies of sedimentary basins can provide information on the nature of depositional systems,on patterns of erosional unroofing,and on kinematic histories of fold-thrust systems Correlation of lithostratigraphic sections can reveal the nature of lateral facies changes in a basin,can provide significant clues for environmental and paleogeographic reconstructions,and may help further understanding basin evolution.However,correlations based solely on lithostratigraphy are often problematic due to the diachroneity of basin infilling by similar lithologic units.True time correlations are those based on更多还原