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《Geology and Exploration》 2011-05
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Chemical Characters and Genesis of Minerals in the Granodiorite-porphyry from the Tongshan Deposit,Anhui Province

LI Da-peng1,DU Yangsong1,ZHANG Jing1,PANG Zhen-shan2,ZHANG Zhi-yu1,JIA Peng-fei1,LI Pin-jie3(1.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083; 2.Development Research Center,China Geological Survey,Beijing 100037; 3.Tongling Nonferrous Metals Group,Tongling,Anhui 247127)  
Chemical characters and genesis of minerals in the granodiorite-porphyry from the Tongshan copper deposit has been investigated in this paper.The result indicates that in this rock the biotite contains 35.75~37.75 wt% SiO2,13.27~13.74 wt% Al2O3,0.00~0.16 wt% MgO,15.33~17.42 wt% FeOT,3.11~4.66 wt% TiO2,and its MF values range from 0.57 to 0.66,dominated by phlogopite.The amphibole contains 36.21~46.91 wt% SiO2,6.26~13.74 wt% Al2O3,12.95~17.19 wt% MgO,13.50~15.33 wt% FeOT,1.10~3.11 wt% TiO2.mostly actinolite and magnesian amphibole.And the biotite comprises 50.49~56.68 wt% SiO2,0.17~1.08 wt% Al2O3,0.00%~3.03 wt% MgO,0.00%~18.24 wt% FeOT,and 0.00%~0.19 wt% TiO2.The parental magma of granodiorite-porphyry in Tongshan is the M-C contamination magma,belonging to subalkaline series,which formed during the late orogenic epoch.The granodiorite-porphyry was formed at temperature 750~900°C and pressure 3.2×108Pa~4×108Pa,at depth of 10.56km~13.2km,and under the condition of high oxygen fugacity.
【Fund】: 全国危机矿山接替资源找矿项目(编号20089938)资助
【CateGory Index】: P618.41
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