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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2009-03
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The palaeolimnological record from Northern Tibet based on trace element chemistry of ostracod shells and the paleoenvironment implication in Tongtianhe basin,Tibet,China

YANG Hong-meiState Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China  
The extensive distribution of lacustrine strata of the Wudaoliang Group indicates a durative,stable paleolake environment in the interior of the Tibetan Plateau during early of Miocene period.To understand the evolution of the environment of the interior of the Tibetan Plateau during this period,the content Mg/Ca and Sr/Ca of ostracod shells from the Wudaoliang Group has been measured.The characteristic of Mg/Ca and Sr/Ca of ostracod shell geochemistry and sedimentology of the measured section located in the Tongtianhe basin reflects that during 23.8~21.8 Ma B.P.,the evolution of the climate in the area experienced the course from wet and wet to dry,at last to warm and wet.The climate change should be the result of the tectonic reactivity after the Tibetan Plateau uplift to denudation and planation.This research explores a new method to study the paleoenvironment in the hinter of the Tibetan Plateau further.
【Fund】: 国家973项目(2006CB701400);; 财政部国家油气专项课题(XQ2004-06)
【CateGory Index】: P595
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