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《Acta Geological Sinica》 2007-01
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~(40)Ar/~(39)Ar Dating of Gold Deposit Hosted in the Daping Ductile Shear Zone in the Ailaoshan Gold Belt, Yunnan Province, China

SUN Xiaoming 1,2), XIONG Dexin 1,3), SHI Guiyong 1), WANG Shengwei 1), ZAI Wei 1) 1) Department of Earth Science, Sun Yat-sen University, Guangzhou, 510275; 2) State Key Laboratory for Mineral Deposits Research, Department of Earth Sciences, Nanjing University, Nanjing, 210093; 3) Zhaoqing University, Zhaoqing, Guangdong, 526061  
Being one of the largest gold deposits in the Ailaoshan gold belt in Yunnan Province, the Daping gold mine occurred in a strongly mylonitized and sericitized Caledonian diorite batholith, and is a typical ductile shear zone-controlled gold deposit. 40Ar/ 39Ar dating was performed on hydrothermal sericite collected from mylonitized and sericitized diorite around rock of the Daping gold deposit, which yielded a set of age data, i.e., plateau age of 33.76±0.65 Ma, inverse and normal isochronal ages of 33.55±0.74 Ma and 33.57±0.74 Ma, respectively. These age data are very similar to ages (33~34 Ma) of the lamprophyre dykes, which are extensively distributed in the Ailaoshan gold belt, suggesting that gold mineralization of the Daping mine was closely related to the Cenozoic lamprophyre dykes, which were generated by partial melting of the upper mantle. From early of the Cenozoic Era, upwelling of the Moho and partially melted upper mantle caused by crustal extension and strong ductile deformation resulted in formation and intrusion of large amounts of lamprophyre dykes. The mantle-derived fluids formed by the upper mantle degassing and the CO_2-riching fluids from the lower crust released by dehydration and roasting triggered by the rising hot mantle magma’s heat mixed and migrated up along micro-fractures in the shear zone, and reacted with the mylonitized and sericitized diorite around rock, and finally deposited the ore minerals in the brittle structures of the shear zone because of water-rock interaction and boiling.
【Fund】: 国家自然科学基金项目(编号40673045、40173025);; 国家重点基础研究发展规划“973”项目(编号2002CB412610);; 国家教育部跨世纪优秀人才培养计划基金项目;; 南京大学成矿作用国家重点实验室开放基金资助的成果
【CateGory Index】: P618.51
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