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《Journal of Changchun University of Science and Technology》 2003-03
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NEW EVIDENCE FROM STABLE ISOTOPE FOR THE UPLIFT OF MOUNTAINS IN NORTHERN EDGE OF THE QINGHAI-TIBETAN PLATEAU

CHEN Zhengle1, WANG Xiaofeng1, FENG Xiahong2, WANG Changqiu3, LIU Jian1(1. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing100081,China; 2. Department of Earth Sciences,Dartmouth College,Hanover,NH03755;3. Department of Geology, Beijing University, Beijing100871,China)  
This work presents a study on the uplift history of mountains in the northern Qinghai-Tibetan Plateau based on evidence of stable isotope ratio of oxygen and carbonate in pedogenic calcite from Jiangeleshayi area, northwestern edge of the plateau. Analysis results showed that rapid changes of δ18O and δ13C in calcite cement occurred both in early Oligocene and early Miocene. The study on sedimentary features indicated that a quick upcoarsing of the sediments size appeared in early Miocene, and sedimentary velocity increased rapidly during Pliocene and early Quaternary. These results suggested that the uplift of mountains in northern edge of the Qinghai-Tibetan Plateau initiated from early Oligocene, and a rapid uplift occurred in early stage of Miocene, while the strongest uplifting occurred from Pliocene to early Quaterary. 
【Fund】: 国家自然科学基金资助项目(40102022);; 国家重点基础研究项目(2001CB409808 01CB7110013)
【CateGory Index】: P542.2
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