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    中国百强科技报刊

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    Volume 38 Issue 4
    Jul.  2013
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    Article Contents
    LIU Fang-xiao, LIU De-min, LI De-wei, ZHOU Tao, DU Cheng-chen, 2013. Causes and Tectonic Evolution of Bangong Lake Basin. Earth Science, 38(4): 745-754. doi: 10.3799/dqkx.2013.072
    Citation: LIU Fang-xiao, LIU De-min, LI De-wei, ZHOU Tao, DU Cheng-chen, 2013. Causes and Tectonic Evolution of Bangong Lake Basin. Earth Science, 38(4): 745-754. doi: 10.3799/dqkx.2013.072

    Causes and Tectonic Evolution of Bangong Lake Basin

    doi: 10.3799/dqkx.2013.072
    • Received Date: 2012-12-04
    • Publish Date: 2013-07-01
    • Causes and tectonic evolution of Bangong lake basin are studied based on the results of geological survey, fluvial sedimentary natures, the age of deposition and its distribution law, referring to ETM+ remote sensing interpretation about tectonics and Quaternary sedimentary strata. Analysis of topography, sedimentary and tectonics indicates that Bangong lake basin is a pull-apart faulted basin; according to activity characteristics of the faults around the lake basin and sedimentary response, the evolution of lake basin is devided into four stages: infancy of lake basin open (later than the early Miocene), adolescence of basin expansion (8.1±1Ma), maturity of rapid expansion of the lake basin with lake basin center moving south (later than 0.94Ma) and gerontic age of lake basin asymmetric atrophy (later than 0.23Ma).

       

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