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《Chinese Journal of Geophysics》 2008-01
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Apatite fission track evidence for two phases Mesozoic-Cenozoic thrust faulting in eastern Qaidam Basin

JIANG Rong-Bao~1, CHEN Xuan-Hua~1, DANG Yu-Qi~2, YIN An~3, WANG Li-Qun~2, JIANG Wu-Ming~2, WAN Jing-Lin~4, LI Li~1, WANG Xiao-Feng~11 Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China2 Qinghai Oilfield Company of PetroChina Company Limited, Dunhuang Gansu 736202, China3 Department of Earth and Space Sciences, University of California, Los Angeles, CA 90095-1567, USA4 Institute of Geology, China Earthquake Administration, Beijing 100029, China  
In eastern Qaidam Basin, the metamorphic and sedimentary Pre-Mesozoic basement had been uplifted due to faulting of the East Qaidam Thrust System and then was separated from the Gonghe Basin due to dextral strike-slip faulting of Wenquan Fault. Apatite fission track analyses and thermochronology of eastern Qaidam Basin show two phases of exhumation and thrusting since Mesozoic. Phase I spanned from 108 Ma to 61 Ma, showing a reduction of AFT cooling ages from south to north, and could be interpreted as the tilting exhumation of the Qaidam basement and thrusting before and at the beginning of Cenozoic. Phase II occurred during 26.6~17.8 Ma between Paleogene and Neogene, which is expressed as the out-of-sequence Cenozoic thrusting of East Qaidam Thrust System.
【Fund】: 国家自然科学基金(40342015);; 国土资源大调查项目(1212010633601)资助
【CateGory Index】: P542
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