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《Acta Geoscientica Sinica》 2012-04
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Mineral Chemical Characteristics of Biotites from Hornfels in the Jiama(Gyama) Polymetallic Copper Deposit of Tibet and Their Geological Significance

WANG Wei-ping 1),TANG Ju-xing 2),YING Li-juan 2) 1) Graduate Department,Chinese Academy of Geological Sciences,Beijing 100037;2) MLR Key Laboratory of Metallogeny and Mineral Resource Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037  
Biotite from hornfels in the Jiama(Gyama) polymetallic copper deposit can be classified into primary biotite and hydrothermal one.Two sorts of biotite were observed by SEM and measured by EMPA.The authors calculated the chemical formula of biotite on the basis of EMPA data.Both primary and hydrothermal biotites are magnesian biotites and have experienced hydrothermal alterations.Magma-hydrothermal fluids were gradually converted into oxidation state,as evidenced by the increase of Fe 3+ and decrease of Fe 2+,the increasing differentiation between Fe 3+ and Fe 2+,and the decrease of K,Na and Ca content from primary biotite to hydrothermal one.Compared with things of primary biotite,more Cu was likely to be concentrated in hydrothermal biotite.The Cu content of rocks has positive correlation with Fe 2+ /(Fe 2+ +Mg 2+) of biotite,and negative correlation with Fe 3+ /Fe 2+ in hydrothermal biotites,which suggests that the mineralization intensity of hornfels-type ores containing hydrothermal biotites might be judged by Fe 2+ /(Fe 2+ +Mg 2+) ratio of hydrothermal biotites;nevertheless,Mo is spread in two sorts of biotite diffusely,and doesn't have characteristics of selective occurrence.
【Fund】: 国家973项目(编号:2011CB403103);; 危机矿山接替资源找矿专项典型矿床及成矿规律总结研究项目(编号:20089932);; 青藏专项(编号:1212010012005)联合资助
【CateGory Index】: P578.959
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