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HOH XIL PIGGYBACK BASINS:IMPLICATIONS FOR PALEOGENE SHORTENING OF THE TIBETAN PLATEAU
作者姓名:Liu Zhifei    Wang Chengshan  Yi Haishen  Liu Shun
作者单位:1 Laboratory of Marine Geology,Tongji University,Shanghai 200092,China,E\|mail: lzhifei@online.sh.cn;2 Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu
摘    要:HOH XIL PIGGYBACK BASINS:IMPLICATIONS FOR PALEOGENE SHORTENING OF THE TIBETAN PLATEAU


HOH XIL PIGGYBACK BASINS:IMPLICATIONS FOR PALEOGENE SHORTENING OF THE TIBETAN PLATEAU
Liu Zhifei ,,Wang Chengshan ,Yi Haishen ,Liu Shun .HOH XIL PIGGYBACK BASINS:IMPLICATIONS FOR PALEOGENE SHORTENING OF THE TIBETAN PLATEAU[J].Earth Science Frontiers,2000(Z1).
Authors:Liu Zhifei  
Institution:Liu Zhifei 1,2,Wang Chengshan 2,Yi Haishen 2,Liu Shun 2
Abstract:Strong deformed sediments investigated in the Hoh Xil basin may contain detailed records for early Tertiary crustal shortening in northern Tibet (Fig.1A). Sedimentary sequences in the basin consist of the Fenghuoshan Group, the Yaxicuo Group, and the early Miocene Wudaoliang Group from lower to upper. Magnetostratigraphic research has indicated the Eocene to early Oligocene ages for the Fenghuoshan and Yaxicuo Groups (Liu, et al., 2000). Total 29 lithological sections with 20487 7m thick were measured spread all over the 101000km\ 2 Hoh Xil basin, the largest Tertiary sedimentary basin in the hinterland of the Tibetan plateau, to reveal the prototype basin and its evolution processes. They include 17 sections with 14925 3m thick of the Fenghuoshan Group, 8 sections with 4273 5m thick of the Yaxicuo Group, and 4 sections with 1284 9m thick of the Wudaoliang Group.
Keywords:piggyback basin  crustal shortening  the Hoh Xil basin  northern Tibet
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