首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Re–Os Age of Molybdenite from the Daheishan Mo Deposit in the Eastern Central Asian Orogenic Belt,NE China
Authors:Chunming Han  Wenjiao Xiao  Brian F Windley  Guochun Zhao  Bexun Su  Songjian Ao  Jien Zhang  Zhiyong Zhang  Bo Wan  Bin Cui  Wenjun Qu  Andao Du
Institution:1. State Key laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, , Beijing, China;2. Department of Geology, University of Leicester, , Leicester, UK;3. Department of Earth Sciences, The University of Hong Kong, , Hong Kong, China;4. China University of Geosciences, , Beijing, China;5. National Research Center of Geoanalysis, , Beijing, China
Abstract:The Daheishan Mo deposit is located in the eastern part of the Central Asian Orogenic Belt, NE China. Rhenium and osmium isotopes of molybdenites from the Daheishan deposit were used to determine the age of mineralization. Rhenium concentrations in molybdenite samples are between 17 and 30μg g?1. Analysis of seven molybdenite samples yields an isochron age of 168.0 ± 4.4 Ma (2σ). Based on the geological history and spatial‐temporal distribution of the granitoids, it is proposed that the Mo deposits in eastern China were related to the subduction of the Paleo‐Pacific plate during Jurassic time.
Keywords:Daheishan  Mo deposit  Re–  Os study  the Central Asian Orogenic Belt
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号