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《Acta Sedimentologica Sinica》 2006-06
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Cenozoic Uplift of West Qinling , Northeast Margin of Tibetan Plateau: The record of detrital apatite fission track data in Tianshui Basin

WANG Xiu-xi 1 LI Ji-jun 1,2 SONG Chun-hui 1 ZHANG Jun 1 ZHAO Zhi-jun 2 GAO Jun-ping 1 PAN Mei-hui 1(1. Key Laboratory of Western Chienese Environmental Systems, Ministry of Education & College of Earth and Environment Sciences, Lanzhou University, Lanzhou 730000; 2 .College of Geography, Nanjing Normal University,Nanjing 210097)  
An important key site in Tianshui Basin which locates between Liupan mountain and west Qinling, northeast margin of Tibetan Plateau exposed a conformable Cenozoic sedimentary sequence that recorded the exhumation history of this area. So, studying these sediments is very important to reveal the tectonic-heating history of this area. Detrital apatite grain thermochronology was used to examine samples of sandstone and conglomerate, sampled from Yaodian section, Tianshui Basin. With othes evidences, we infered two tectonic-heating events occurred at the source regions of the Tianshui Basin. One event, the tectonic uplift of west Qinling, occurred at about 23.7Ma and had the relationship with the Tibetan plateau uplift, which resulted in the formation of Tianshui Basin and to start alluvial deposits in Tianshui Basin. Another tectonic event occured at about 14.1Ma, which made Tianshui Basin was depressed again and came into being broad fluvio-lacustrine deposits. The source region uplifted and were eroded rapidly because of the events. The rough mean exhumation rates were 0.34mm/a and 1.05mm/a ,respectively.
【Fund】: 国家重点基础研究发展计划(973计划)项目(批准号:2005CB422001);; 国家自然科学基金(批准号:90211013 40421101)资助.
【CateGory Index】: P542.1
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