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《World Sci-tech R & D》 2007-02
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Fission Track Thermochronology Application to Mineralization Ages of Hydrothermal Deposits in Kelang Basin,Northern Xinjiang,China

YUAN Wanming1 BAO Zengkuan2 DONG Jinquan2 AN Yinchang3(1.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083;2.Key Laboratory of Nuclear Analysis Techniques,Institute of High Energy Physics,Chinese Academy of Sciences,Beijing 100049;3.Institute of Exploration of Nonferrous Metal Geology and Mineral Resources,Xinjiang Uygur Autonomous Region,Urumchi 830000)  
It is a new attempt to apply Fission track thermochronology to mineralization field and it is feasible because the homogenization temperature of metallogenic fluid inclusions from different ore deposits in Kelang basin,northern Xinjiang ranges from 105 ℃ to 294 ℃ and accords with the retentions temperature of fission tracks in zircon and apatite on the whole.This study has achieved 6 zircon and 17 apatite fission track analysis results.The zircon fission track ages range from 134 Ma to 312 Ma and are divided into three groups of 312 Ma,247 Ma and 158-134 Ma.We consider that the three age groups reflect three metallogenic epochs.The apatite ages are between 30 Ma and 130 Ma,belong to end of the metallogenic thermal events.Consequently,the mineralization occurred not only in Hercynian and Indosinian epochs,but also in Yanshanian epoch,even in Himalayan epochs.
【Fund】: 国家自然科学基金资助项目(40072068 10175076 10475093);; 国家重点基础研究发展规划项目(2001CB409804);; 国家科技攻关项目(2001BA609A-07-03)
【CateGory Index】: P612
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