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胶东三山岛金矿中深部成矿流体对比及矿床成因
引用本文:姜晓辉,范宏瑞,胡芳芳,杨奎锋,蓝廷广,郑小礼,金念宪. 胶东三山岛金矿中深部成矿流体对比及矿床成因[J]. 岩石学报, 2011, 27(5): 1327-1340
作者姓名:姜晓辉  范宏瑞  胡芳芳  杨奎锋  蓝廷广  郑小礼  金念宪
作者单位:1. 中国科学院地质与地球物理研究所,矿产资源研究重点实验室,北京,100029
2. 山东黄金集团有限公司,莱州,264000
基金项目:本文受国家自然科学基金项目(40625010)和全国危机矿山接替资源找矿项目(20089930)联合资助.
摘    要:三山岛金矿位于胶东西北部,属于典型的破碎蚀变岩型金矿。流体包裹体研究表明该矿床为中温、中低盐度H2O-CO2-NaCl±CH4流体;中深部成矿流体对比研究表明,在纵深超过2000m范围内,成矿流体具有较一致的成矿流体介质条件,主成矿均一温度为170~330℃,成矿压力为50~255MPa。H、O、C同位素表明,深源流体参与了成矿作用,很可能是与金矿床伴生的基性幔源岩浆脱水形成的岩浆水,在地壳浅部遭受到大气降水的混合,而S同位素研究进一步揭示了成矿物质具有多源性,矿区浅表在成矿晚期可能受到了表生硫影响而导致δ34S偏高。水岩反应、成矿应力场转变及表面吸附电化学还原反应等导致金沉淀成矿。

关 键 词:流体包裹体  稳定同位素  深部矿体  破碎蚀变岩型  三山岛金矿  胶东
收稿时间:2011-01-06
修稿时间:2011-03-31

Comparative studies on fluid inclusion in different depths and ore genesis of the Sanshandao gold deposit, Jiaodong Peninsula.
JIANG XiaoHui,FAN HongRui,HU FangFang,YANG KuiFeng,LAN TingGuang,ZHENG XiaoLi and JIN NianXian. Comparative studies on fluid inclusion in different depths and ore genesis of the Sanshandao gold deposit, Jiaodong Peninsula.[J]. Acta Petrologica Sinica, 2011, 27(5): 1327-1340
Authors:JIANG XiaoHui  FAN HongRui  HU FangFang  YANG KuiFeng  LAN TingGuang  ZHENG XiaoLi  JIN NianXian
Affiliation:Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Shandong Gold Company Ltd., Laizhou 264000, China;Shandong Gold Company Ltd., Laizhou 264000, China
Abstract:
Keywords:Fluid inclusion  Stable isotopes  Deep ore bodies  Disseminated and stockwork style  Sanshandao gold deposit  Jiaodong
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