吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (5): 1552-1569.doi: 10.13278/j.cnki.jjuese.20200120

• 整装勘查区矿床成因与成矿作用研究专辑 • 上一篇    下一篇

山东栖霞笏山金矿床成因——元素地球化学与流体包裹体证据

智云宝1, 孙海瑞2,3, 李风华1   

  1. 1. 山东省地质调查院, 济南 250013;
    2. 中国地质调查局发展研究中心, 北京 100037;
    3. 自然资源部矿产勘查技术指导中心, 北京 100083
  • 收稿日期:2020-05-13 出版日期:2020-09-26 发布日期:2020-09-29
  • 通讯作者: 孙海瑞(1987-)男,高级工程师,博士,主要从事岩石学及矿床学方面的研究,E-mail:HaiRuiSun@126.com E-mail:HaiRuiSun@126.com
  • 作者简介:智云宝(1978-)男,高级工程师,硕士,主要从事矿产资源勘查研究及潜力评价方面的研究,E-mail:27516999@qq.com
  • 基金资助:
    中国地质调查局项目（121201004000150017-60，DD20190159）；国家重点研发计划项目（2016YFC0600107）；山东省地质勘查项目（鲁勘字（2018）19号，鲁勘字（2019）1号）

Geological and Geochemical Features of Hushan Gold Deposit in Qixia, Shandong Province

Zhi Yunbao1, Sun Hairui2,3, Li Fenghua1   

  1. 1. Institute of Geological Survey, Shandong Province, Jinan 250013, China;
    2. Development and Research Center, China Geological Survey, Beijing 100037, China;
    3. Mineral Exploration Technical Guidance Center, Ministry of Natural Resources, Beijing 100083, China
  • Received:2020-05-13 Online:2020-09-26 Published:2020-09-29
  • Supported by:
    Supported by Project of China Geological Survey (121201004000150017-60,DD20190159),National Key R&D Program of China(2016YFC0600107) and Geological Exploration Projects in Shandong Province (LKZ (2018)No.19,LKZ (2019) No.1)

PDF (PC)

244

摘要： 笏山金矿床为陡崖断裂带南段内最大的金矿床，为了揭示其矿床成因，在矿床地质研究的基础上开展了矿体围岩元素地球化学和流体包裹体研究。研究结果表明：笏山金矿床沿NE向断裂发育大规模的热液蚀变带，地表出露的断裂带形成一个庞大的面形蚀变带，矿化较弱，分带不明显，钻孔显示金矿体两侧依次发育黄铁绢英岩、绢英岩化花岗岩蚀变带和二长花岗岩，金矿体主要产于陡崖断裂带下盘黄铁绢英岩蚀变带内。质量平衡计算表明：绢英岩化过程中，主量元素SiO2、Al2O3、FeO、MnO、Na2O、K2O、P2O5和部分稀土元素从二长花岗岩中迁出，而MgO、CaO、Fe2O3，成矿元素Au、Ag，亲硫元素Cu、Pb及亲铁元素V、Cr、Co、Ni迁入二长花岗岩；黄铁绢英岩化过程中，主量元素FeO、Fe2O3、MnO、MgO、CaO，成矿元素Au、Ag，亲硫元素Cu及亲铁元素V、Cr、Co、Ni迁入，SiO2、Al2O3、Na2O、K2O和P2O5迁出。岩相学观察、显微测温以及单个包裹体成分激光拉曼分析提示其流体包裹体类型主要为气液两相包裹体和含CO2三相包裹体，具有低盐度（w（NaCl）为5.33%~13.29%）和中温（260~300℃）CO2-NaCl-H2O体系，在成矿过程中，含矿流体经历了流体不混溶作用。结合矿床地质特征及实验结果分析，确定该矿床为受陡崖断裂带控制的中温蚀变岩型金矿床。

关键词: 笏山金矿床, 热液蚀变, 成矿流体, 栖霞, 胶东

Abstract: Hushan gold deposit is the largest gold deposit in the southern part of Douya fault. In order to reveal its genesis, based on the geological work of the deposit, the study of the surrounding rock element geochemistry and fluid inclusions of the ore body was carried out. The results show that a large-scale of hydrothermal alteration is developed along the NE-trending faults in Hushan Au deposit,with obvious surface hydrothemal alteration, low Au mineralization, and poor alteration zoning. The borehole logs show that the hydrothermal alteration along the Au ore-bodies is symmetrically developed, displaying sericite-quartz alteration and pyrite-sericite-quartz alteration with the increase of distance from ore-body. The ore-bodies are mainly hosted in the alteraltion zone of pyrite-sericite-quartz alteration at the footwall of Douya fault. The mass-balance calculation shows that the major and trace elements behaved complicatedly during fluid-rock interaction. In the stage of sericite-quartz alteration, Linglong biotite granite experienced the loss of SiO2, Al2O3, FeO,MnO, Na2O, K2O, P2O5, and enrichment of REEs and MgO, CaO, Fe2O3, Au, Ag, Cu, Pb, V, Cr, Co and Ni; in the stage of pyrite-sericite-quartz alteration, FeO, Fe2O3, MnO, MgO, CaO, Au, Ag, Cu, V, Cr, Co, and Ni enterred in the sericite- quartz altered granite, while SiO2, Al2O3, Na2O, K2O and P2O5 moved out. The petrographic, microthermometric, and laser Raman microspectroscopic analyses on the fluid inclusions show that the fluid inclusions are mainly two-phrase aqueous fluid inclusions and CO2-bearing three phase inclusions, which are low salinity (5.33%-13.29%) and medium temperature (260 to 300 ℃) CO2-NaCl-H2O system. The ore fluid experienced fluid immiscibility during the ore-forming process. We believe that the deposit should belong to mesothermal altered rock type Au deposit controlled by Douya fault, which is similar to Jiaojia Au deposit in Jiaodong area.

Key words: Hushan gold deposit, hydrothermal alteration, ore-forming fluid, Qixia, Jiaodong

中图分类号: 

  • P611
[1] 于学峰,李大鹏,田京祥,等.山东金矿深部勘查进展与成矿理论创新[J].山东国土资源,2018,34(5):1-13. Yu Xuefeng,Li Dapeng, Tian Jingxiang,et al. Progress of Deep Exploration and Theoretical Innovation of Metallogenic of Gold Deposits in Shandong Province[J]. Shandong Land and Resources, 2018,34(5):1-13.
[2] 宋明春,李三忠,伊丕厚,等.中国胶东焦家式金矿类型及其成矿理论[J].吉林大学学报(地球科学版),2014,44(1):87-104. Song Mingchun,Li Sanzhong,Yi Pihou,et al. Classification and Metallogenic Theory of the Jiaojia Style Gold Deposit in Jiaodong Peninsula,China[J]. Journal of Jilin University(Earth Science Edition),2014,44(1):87-104.
[3] Song Mingchun,Li Sanzhong,Santosh M,et al. Types,Characteristics and Metallogenesis of Gold Deposits in the Jiaodong Peninsula,Eastern North China Craton[J]. Ore Geology Reviews,2015,65:612-625.
[4] Yang Liqiang,Deng Jun,Wang Zhongliang,et al. Mesozoic Gold Metallogenic System of the Jiaodong Gold Province,Eastern China[J]. Acta Petrologica Sinica,2014,30(9):2447-2467.
[5] Deng Jun,Liu Xuefei,Wang Qingfei,et al. Origin of the Jiaodong-Type Xinli Gold Deposit,Jiaodong Peninsula, China:Constraints from Fluid Inclusion and C-D-O-S-Sr Isotope Compositions[J]. Ore Geology Reviews,2015,65:674-686.
[6] Zhang Binglin,Shan Wei,Li Dapeng,et al. Hydrothermal Alteration in the Dayingezhuang Gold Deposit, Jiaodong, China[J]. Acta Petrologica Sinica,2017,33(7):2256-2272.
[7] Yang Liqiang,Deng Jun,Wang Zhongliang,et al. Thermochronologic Constraints on Evolution of the Linglong Metamorphic Core Complex and Implications for Gold Mineralization:A Case Study from the Xiadian Gold Deposit,Jiaodong Peninsula,Eastern China[J]. Ore Geology Reviews,2016,72:165-178.
[8] 庞绪成,王玉平,郑广玉,等.焦家金矿床成矿元素富集及成因分析[J].黄金科学技术,2003,11(2):15-19. Pang Xucheng,Wang Yuping,Zheng Guangyu,et al. Analysis of Ore-Formation and Elements Concentration in Jiaojia Gold Deposit[J]. Gold Science & Technology, 2003,11(2):15-19.
[9] Deng Jun, Yang Liqiang,Sun Zhongshi,et al. A Metallogenic Model of Gold Deposits of the Jiaodong Granite-Greenstone Belt[J]. Acta Geologica Sinica,2003,77(4):537-546.
[10] 罗镇宽,苗来成.胶东招莱地区花岗岩与金矿[M].北京:冶金工业出版社,2002. Luo Zhenkuan,Miao Laicheng. Granite and Gold Mine in Zhaolai Area,Jiaodong Region[M]. Beijing:Metallurgical Industry Press,2002.
[11] 凌洪飞,胡受奚,孙景贵,等.胶东金青顶和大尹格庄金矿床花岗质围岩的蚀变地球化学研究[J].矿床地质,2002,21(2):187-197. Ling Hongfei,Hu Shouxi,Sun Jinggui,et al. Geochemical Study of Granitic Wall Rock Alteration in Dayingezhuang Gold Deposit of Alteration Rock Type and Jinqingding Gold Deposit of Quartz Vein Type[J]. Mineral Deposits,2002,21(2):187-197.
[12] 陈海燕,李胜荣,张秀宝,等.胶东金青顶金矿床围岩蚀变特征与金矿化[J].矿物岩石地球化学通报,2002,31(1):5-13. Chen Haiyan,Li Shengrong,Zhang Xiubao,et al. Wall Rock Alteration and Gold Mineralization in the Jinqingding Gold Deposit,Eastern Shandong Province[J]. Bulletin of Mineralogy,Petrology and Geochemistry,2002,31(1):5-13.
[13] Li Xiaochun,Fan Hongrui,Santosh M,et al. Hydrothermal Alteration Associated with Mesozoic Granite-Hosted Gold Mineralization at the Sanshandao Deposit,Jiaodong Gold Province,China[J]. Ore Geology Reviews,2013,53:403-421.
[14] 张炳林,杨立强,黄锁英,等.胶东焦家金矿床热液蚀变作用[J].岩石学报,2014,30(9):2533-2545. Zhang Binglin,Yang Liqiang, Huang Suoying,et al. Hydrothermal Alteration in the Jiaojia Gold Deposit, Jiaodong,China[J]. Acta Petrologica Sinica,2014,30(9):2533-2545.
[15] 李士先,刘长春,安郁宏,等.胶东金矿地质[M].北京:地质出版社,2007. Li Shixian,Liu Changchun, An Yuhong,et al. Geology of Gold Deposits in Shandong Peninsula[M]. Beijing:Geological Publishing House,2007.
[16] 杨忠芳,徐景奎,赵伦山.胶东区域地壳演化与金矿成矿作用地球化学[M].北京:地质出版社,1998. Yang Zhongfang,Xu Jingkui,Zhao Lunshan. The Evolution of Regional Crust and the Geochemistry on Gold Mineralization Jiaodong[M]. Beijing:Geological Publishing House,1998.
[17] 杨敏之.金矿床围岩蚀变带地球化学:以胶东金矿为例[M].北京:地质出版社,1998. Yang Minzhi.The Geochemistry of Wall Rock Alteration Zone of Gold Deposits:As Exemplified by Jiaodong Gold Deposits[M]. Beijing:Geological Publishing House,1998.
[18] 钱建平,陈宏毅,孙涛,等.山东招远前孙家金矿床地质和元素地球化学研究[J].地球化学,2010,39(3):213-228. Qian Jianping,Chen Hongyi,Sun Tao,et al. Study on Geology and Element Geochemistry of Qiansunjia Gold Mine in Zhaoyuan, Shandong,Eastern China[J]. Geochimica,2010,39(3):213-228.
[19] 丁式江,翟裕生,邓军.胶东焦家金矿蚀变岩中元素的质量迁移[J].地质与勘探,2000,36(4):28-31. Ding Shijiang,Zhai Yusheng,Deng Jun. Mass Transfer of Altered Rocks in Jiaojia Gold Deposit,Jiaodong[J]. Geology and Exploration,2000,36(4):28-31.
[20] 方金云,孙景瑜.胶东望儿山金矿床成矿过程中物质迁移研究[J].黄金,2000,21(9):1-4. Fang Jinyun,Sun Jingyu. Study on Mass Transfer in the Process of Mineralization of Wangershan Gold Deposit,East Shandong[J]. Gold,2000,21(9):1-4.
[21] 李杰,宋明春,李世勇,等.胶东大邓格金多金属矿床地质地球化学特征及意义[J].中国地质,2016,43(1):221-237. Li Jie,Song Mingchun.Li Shiyong,et al. Geological and Geochemical Features of the Dadengge Gold Polymetallic Deposit in Jiaodong Peninsula[J]. Geology in China,2016,43(1):221-237.
[22] 史宏江.山东栖霞马家疃金矿区地质特征及找矿前景[J].山东国土资源,2016,32(10):5-11. Shi Hongjiang. Geological Characteristics and Prospecting Potential of Majiatuan Gold Mining Area in Qixia City of Shandong Province[J]. Shandong Land and Resources,2016,32(10):5-11.
[23] 谢军民,肖翔,史宏江,等.栖霞市西陡崖矿床地质特征及找矿方向[J].山东国土资源,2011,27(6):1-5. Xie Junmin,Xiao Xiang,Shi Hongjiang,et al. Geological Characteristics and Exploration Direction of Xidouya Deposit in Qixia City of Shandong Province[J]. Shandong Land and Resources,2011,27(6):1-5.
[24] 许方.山东省栖霞台前金矿床地质特征及找矿方向[J].地质找矿论从,2008,23(2):140-143. Xu Fang. Geological Characteristics of Taiqian Gold Deposit and the Ore-Seaching Dirction in the Mining District[J]. Contributions to Geology and Mineral Resources Research,2008,23(2):140-143.
[25] 廖明伟,陈玉菡,谢军民.山东省栖霞市笏山-西陡崖金矿地质特征及深部找矿远景[J].山东国土资源,2014,30(4):21-24. Liao Mingwei,Chen Yuhan,Xie Junmin. Geological Characteritics and Deep Gold Prospecting of Hushan-Xidouya Gold Deposit in Qixia City of Shandong Province[J]. Shandong Land and Resources, 2014,30(4):21-24.
[26] 宋明春,徐军祥,王沛成.山东省大地构造格局和地质构造演化[D].北京:中国地质科学院,2008. Song Mingchun,Xu Junxiang,Wang Peicheng. Geotectonic Pattern and Evolution in Shandong Province[D]. Beijing:Chinese Academy of Geological Sciences,2008.
[27] 宋明春.胶东金矿深部找矿主要成果和关键理论技术进展[J].地质通报,2015,34(9):1758-1771. Song Mingchun. The Main Achievements and Key Theory and Methods of Deep-Seated Prospecting in the Jiaodong Gold Concentration Area, Shandong Province[J]. Geological Bulletin of China,2015,34(9):1758-1771.
[28] 王瑞良,张招崇,曾庆栋,等.胶东栖霞金矿集区早白垩世花岗岩形成时代及地质意义[J].大地构造与成矿学,2019,43(1):186-198. Wang Ruiliang,Zhang Zhaochong,Zeng Qingdong,et al. Ages of the Early Cretaceous Granites in Qixia Gold Concentration Area,Shandong Province and Implications for Gold Mineralization[J]. Geotectonica et Metallogenia, 2019,43(1):186-198.
[29] 宋明春,宋英昕,李杰,等.胶东与白垩纪花岗岩有关的金及有色金属矿床成矿系列[J].大地构造与成矿学,2015,39(5):833-835. Song Mingchun,Song Yingxin, Li Jie,et al. Metallogenic Series of Gold and Nonferrous Metal Deposits Related to Cretaceous Granites in Eastern Shandong Peninsula, China[J]. Geotectonica et Metallogenia, 2015,39(5):833-835.
[30] 罗镇宽,苗来成.胶东招莱地区花岗岩与金矿[M].北京:冶金工业出版社,2002. Luo Zhenkuan,Miao Laicheng. Granite and Gold Mine in Zhaolai Area,Jiaodong Region[M]. Beijing:Metallurgical Industry Press,2002.
[31] 苗来成,罗镇宽,关康,等.玲珑花岗岩中锆石的离子质谱U-Pb年龄及其岩石学意义[J].岩石学报,1998,14(2):198-206. Miao Laicheng,Luo Zhenkuan,Guan Kang,et al. The Implication of the SHRIMP U-Pb Age in Zircon to the Petrogenesis of the Linglong Granite,East Shangdong Province[J]. Acta Petrologica Sinica,1998,14(2):198-206.
[32] 宋雪龙,李俊建,李秀章,等.胶东金矿床成矿流体、稳定同位素及成矿时代研究进展[J].地质找矿论丛,2014,29(1):13-19. Song Xuelong,Li Junjian,Li Xiuzhang,et al. The Research Progress of Ore-Forming Fluids,Stable Isotope and Mineralizing Age in Jiaodong Peninsular of Eastern China[J]. Contributions to Geology and Mineral Resources Research,2014,29(1):13-19.
[33] 陈广俊,孙丰月,李玉春,等.胶东郭家岭花岗闪长岩U-Pb年代学、地球化学特征及地质意义[J].世界地质,2014,33(1):39-47. Chen Guangjun,Sun Fengyue,Li Yuchun,et al. U-Pb Dating,Geochemical Characteristics and Geological Significance of Guojialing Grandiorite in Jiaodong Peninsula[J]. Global Geology,2014,33(1):39-47.
[34] 关康,罗镇宽,苗来成,等.胶东招掖郭家岭型花岗岩锆石SHRIMP年代学研究[J].地质科学,1998,33(3):318-328. Guan Kang,Luo Zhenkuan,Miao Laicheng,et al. SHRIMP in Zircon Chronology for Guojialing Suite Granite in Jiaodong Zhaoye District[J]. Scientia Geologica Sinica,1998,33(3):318-328.
[35] Deng Jun, Liu Xuefei, Wang Qingfei,et al. Isotopic Characterization and Petrogenetic Modeling of Early Cretaceous Mafic Diking:Lithospheric Extension in the North China Craton,Eastern Asia[J]. GSA Bulletin,2017,129(11/12):1379-1407.
[36] 宋明春,宋英昕,丁正江,等.胶东焦家和三山岛巨型金矿床的发现及有关问题讨论[J].大地构造与成矿学,2019,43(1):92-110. Song Mingchun,Song Yingxin,Ding Zhengjiang,et al. The Discovery of the Jiaojia and the Sanshandao Giant Gold Deposits in Jiaodong Peninsula and Discussion on the Relevant Issues[J]. Geotectonica et Metallogenia,2019,43(1):92-110.
[37] 徐萌.山东省栖霞市笏山金矿构造特征及其成矿作用分析[D].石家庄:河北地质大学:2016. Xu Meng.The Analysis of the Structural Feature and the Mineralization of Hushan Goldfield in Qixia Shandong Province[D]. Shijiazhuang:Hebei GEO University:2016.
[38] 原丽媛,许凯磊,田少斌.山东省栖霞市笏山-西陡崖金矿集区综合研究报告[R].烟台:山东省核工业二七三地质大队,2018. Yuan Liyuan,Xu Kailei,Tian Shaobin. Comprehensive Study Report on Hushan-Xidouya Gold Deposit in Qixia,Shandong Province[R]. Yantai:Shandong Province Nuclear Industry Geological Group 273,2018.
[39] 廖小明,谢军民,康桂铭,等. 山东省栖霞市笏山矿区金矿详查报告[R].济南:山东省国土资源厅,2012. Liao Xiaoming,Xie Junmin,Kang Guiming,et. Detailed Survey Report of Hushan Gold Deposit in Qixia,Shandong Province[R]. Jinan:Shandong Procincial Department of Land and Resources,2012.
[40] 硅酸盐岩石化学分析方法:第28部分:16个主次成分量测定:GB/T 14506.28-2010[S].北京:中国质检出版社,2010. Methods for Chemical Analysis of Silicate Rocks:Part 28:Determination of 16 Major and Minor Elements Content:GB/T 14506.28-2010[S]. Beijing:China Zhijian Publishing House,2010.
[41] 硅酸盐岩石化学分析方法:第30部分:44个元素量测定:GB/T 14506.30-2010[S].北京:中国质检出版社,2010. Methods for Chemical Analysis of Silicate Rocks:Part 30:Determination of 44 Elements:GB/T 14506.30-2010[S]. Beijing:China Zhijian Publishing House,2010.
[42] Sun S S, Mcdonough W F. Chemical and Isotopic Systematics of Oceanic Basalts;Implications for Mantle Composition and Processes[J]. Geological Society London Special Publications,1989,42(1):313-345.
[43] 卢焕章,范宏瑞,倪培,等.流体包裹体[M]北京:科学出版社,2004. Lu Huanzhang, Fan Hongrui, Ni Pei, et al. The Fluid Inclusion[MJ. Beijing:Science Press, 2004. \
[44] 马芳,孙丰月,霍亮,等.山东焦家金矿煌斑岩特征及金矿化关系[J].世界地质,2014,33(2):388-398. Ma Fang,Sun Fengyue,Huo Liang, et al. Lamprophyre Characteristics and Their Relation to Gold Mineralization of Jiaojia Gold Deposit,Shandong[J]. Global Geology,2014,33(2):388-398.
[45] 王力,孙丽伟.山东省寺庄金矿床成矿流体特征[J].吉林大学学报(地球科学版),2016,46(6):1697-1710. Wang Li,Sun Liwei. Characteristics of Ore-Forming Fluid of the Sizhuang Gold Deposit in Shandong Province[J]. Journal of Jilin University(Earth Science Edition),2016,46(6):1697-1710.
[46] 刘斌,段光贤.NaCl-H2O溶液包裹体的密度式和等容式及其应用[J].矿物学报,1987,7(4):345-352. Liu Bin,Duan Guangxian. The Density and Isochoric Formulae for NaCl-H2O Fluid Inclusions(Salinity ≤ 25wt%) and Their Applications[J]. Acta Mineralogical Sinica, 1987,7(4):345-352.
[47] 桂飞,王力,马芳.三山岛金矿床流体包裹体研究[J].黄金地质,2014,11(35):27-32. Gui Fei,Wang Li,Ma Fang. Study on Fluid Inclusions in the Sanshandao[J]. Gold Geology, 2014,11(35):27-32.
[48] 张文淮,陈紫英.流体包裹体地质学[M].武汉:中国地质大学出版社,1993. Zhang Wenhuai,Chen Ziying. Fluid Inclusions Geology[M]. Wuhan:China University of Geoscience Press,1993.
[49] 刘斌,沈昆.流体包裹体热力学[M].北京:地质出版社,1999. Liu Bin,Shen Kun. Fluide Inclusions Thermodynamics[M]. Beijing:Geological Publishing House,1999.
[50] 王力,潘忠翠,孙丽伟.山东莱州新城金矿床流体包裹体[J].吉林大学学报(地球科学版),2014,46(4):1166-1176. Wang Li, Pan Zhongcui,Sun Liwei. Fluid Inclusions of the Xincheng Gold Deposit of Laizhou City in Shandong Province[J]. Journal of Jilin University(Earth Science Edition),2014,46(4):1166-1176.
[51] 王力,孙丰月,王佳良. 山东金岭金矿床成矿流体地球化学特征[J].岩石学报,2010,26(12):3735-3744. Wang Li,Sun Fengyue,Wang Jialiang. Geochemical Features of Ore-Forming Fluids of the Jinling Gold Deposit in Shandong Province[J]. Acta Petrologica Sinica,2010,26(12):3735-3744.
[52] Fan Hongrui,Hu Fangfang,Yang Jinhui,et al. Fluid Evolution and Large-Scale Gold Metallogeny During Mesozoic Tectonic Transition in the Jiaodong Peninsula,Eastern China.[J]. Geological Society, London, Special Publications 2007,280:303-306.
[53] Fan Hongrui,Zhai Mingguo,Xie Yihan,et al. Ore-Forming Fluids Associated with Granite-Hosted Gold Mineralization at the Sanshandao Deposit,Jiaodong Gold Province[J]. Mineralium Deposita,2003,38:739-750.
[54] 卢焕章,Guha J,方根保.山东玲珑金矿的成矿流体特征[J].地球化学,1999,28(5):421-437. Lu Huanzhang, Guha J,Fang Genbao. Characteristics of Ore-Forming Fluid in Linglong Gold Mine,Shandong, China[J]. Geochimica,1999,28(5):421-437.
[55] 沈昆,胡受奚,孙景贵,等.山东招远大尹格庄金矿成矿流体特征[J].岩石学报,2000,16(4):542-550. Shen Kun,Hu Shouxi,Sun Jinggui,et al. Characteristics of Ore-Forming Fluids of the Dayingezhuang Gold Deposit in Eastern Shandong,China[J]. Acta Petrologica Sinica,2000,16(4):542-550.
[56] 徐九华,何知礼,谢玉玲.绿岩型金矿床成矿流体的地球化学[M].北京:地质出版社,1996. Xu Jiuhua,He Zhili,Xie Yuling. Geochemistry of Ore-Forming Fluids in Greenstone Type Gold Deposits[M]. Beijing:Geological Publishing House, 1996.
[57] 杨忠芳,赵伦山,周奇明,等.胶东牟乳金矿带浅成热液金矿成矿作用的物理化学条件制约[J].矿物学报,1994,14(3):270-278. Yang Zhongfang,Zhao Lunshan,Zhou Qiming,et al. Physicochemtcal Constrains on Mineralization of Epithermal Gold Deposits in Muping-Rushan Mineralization Zone,Eastern Shandong Province,China[J]. Acta Mineralogica Sinica,1994,14(3):270-278.
[58] Grant J A. The Isocon Diagram:A Simple Solution to Gresens Equation for Metasomatic Alteration[J]. Economic Geology,1986,81(8):1976-1982.
[59] Gresens R L. Composition-Volume Relationships of Metasomatism[J]. Chemical Geology,1967,2:47-65.
[60] Grant J A.Isocon Analysis:A Brief Review of the Method and Applications[J]. Physics and Chemistry of the Earth:Parts A/B/C,2005,30(17/18):997-1004.
[61] Barton M D,Ilchik R P,Marikos M A. Contact Metamorphism[J]. Reviews in Mineralogy and Geochemistry,1991,26(1):321-349.
[62] Condie K C,Sinha A K. Rare Earth and Other Trace Element Mobility During Mylonitization:Acomparison of the Brevasrd and Hope Valley Shear Zones in the Appalachian Mountains[J]. USA Journal of Metamorphic Geology,1996,14(2):213-226.
[63] Ague J J. Mass Transfer During Barrovian Metamorphism of Pelites,South-Central Connecticut:I:Evidence for Changes in Composition and Volume[J]. American Journal of Science,1994,294(8):989-1057
[64] O'Hara K, Blackburn W H. Volume-Loss Model for Trace Element Enrichments in Mylonite[J]. Geology,1989,17(6):524-527.
[65] 刘向东,邓军,张良,等.胶西北寺庄金矿床热液蚀变作用[J].岩石学报,2019,35(5):1551-1565. Liu Xiangdong,Deng Jun,Zhang Liang,et al. Hydrothermal Alteration of the Sizhuang Gold Deposit,Northwestern Jiaodong Peninsula,Eastern China[J]. Acta Petrologica Sinica,2019, 35(5):1551-1565.
[66] 张炳林,杨立强,黄锁英,等.胶东焦家金矿床热液蚀变作用[J].岩石学报,2014,30(9):2533-2545. Zhang Binglin,Yang Liqiang,Huang Suoying,et al. Hydrothermal Alteration in the Jiaojia Gold Deposit,Jiaodong,China[J]. Acta Petrologica Sinica,2014,30(9):2533-2545.
[67] 邓军,刘伟,孙忠实,等.幔源流体判别标志及多层循环成矿作用动力学:以山东夏甸金矿床为例[J].中国科学:D辑:地球科学,2003,32(增刊1):96-104. Deng Jun,Liu Wei,Sun Zhongshi,et al. Diagnostic Criterica Mantle Fluids and Dynamics of Multi-Layer Cyclic Mineralization:A Case Study of Xiadian Gold Deposit,Shandong Province[J]. Chinese Science:Series D:Journal of Earth Science,2003,32(Sup.1):96-104.
[68] 张群喜,孙忠实.山东夏甸金矿幔源流体初探[J].地球学报,2003,24(2):127-131. Zhang Qunxi,Sun Zhongshi.A Tentative Discussion on Mantle Fluids in the Xiadian Gold Deposit,Shandong Province[J]. Acta Geoscientia Sinica,2003,24(2):127-131.
[69] Roedder Bodnar K J. Geologic Pressure Determinations from Fluid Inclusion Studies[J]. Annual Review of Earth and Planetary Sciences,1980,8:263-301.
[70] 孙丰月,金巍,李碧乐,等.关于脉状热液金矿床成矿深度的思考[J].长春科技大学学报,2000,30(增刊1):27-30. Sun Fengyue, Jin Wei, Li Bile, el al. Considerations on the Mineralizing Depth of Hydrolhermal Lode Gold Deposits[J]. Journal of Changchun University of Science and Technology,2000,30(Sup.1):27-30.
[71] 宋明春,宋英昕,丁正江,等. 胶东金矿床:基本特征和主要争议[J].黄金科学技术,2018,26(4):406-422. Song Mingchun,Song Yingxin,Ding Zhengjiang,et al. Jiaodong Gold Deposits:Essential Characteristics and Major Controversy[J]. Gold Science and Technology, 2018,26(4):406-422.
[72] 李洪奎,李大鹏,耿科,等.胶东地区燕山期岩浆活动及其构造环境:来自单颗锆石SHRIMP年代学的记录[J].地质学报,2017,91(1):163-179. Li Hongkui,Li Dapeng,Geng Ke,et al. The Mesozoic Magmaticactivities Framework in Jiaodong Area:SHRIMP Chronology Recording of Single Particle Zircon[J]. Acta Geologica Sinica,2017,91(1):163-179.
[73] 杨立强,邓军,王中亮,等.胶东中生代金成矿系统[J].岩石学报,2014,30(9):2447-2467. Yang Liqiang,Deng Jun,Wang Zhongliang, et al. Mesozoic Gold Metallogenic System of the Jiaodong Gold Province, Eastern China[J]. Acta Petrologica Sinica,30(9):2447-2467.
[74] 李洪奎,时文革,李逸凡,等.山东胶东地区金矿成矿时代研究[J].黄金科学技术,2013,21(3):1-9. Li Hongkui,Shi Wenge,Li Yifan, et al. Study on Gold Mineralization Ages in Jiaodong Area, Shandong Province[J]. Gold Science & Technology, 2013,21(3):1-9.
[1] 孙丰月, 王睿, 王一存, 李顺达, 王可勇, 石开拓, 孙清飞, 王文元. 内蒙古碾子沟钼矿床成矿流体来源、演化及成矿机理[J]. 吉林大学学报(地球科学版), 2020, 50(3): 768-780.
[2] 易海永, 崔宝琛, 王瑶琳, 邱玉超, 徐胜林, 李乾. 四川盆地广安地区中二叠统栖霞组岩石特征与沉积环境[J]. 吉林大学学报(地球科学版), 2020, 50(2): 454-464.
[3] 沈崇辉, 赵恩全. 安徽省笔架山绿松石矿床矿石矿物特征及矿床成因[J]. 吉林大学学报(地球科学版), 2019, 49(6): 1591-1606.
[4] 吴永涛, 韩润生. 滇东北矿集区茂租铅锌矿床地球化学特征[J]. 吉林大学学报(地球科学版), 2019, 49(2): 400-413.
[5] 李向文, 张志国, 王可勇, 孙加鹏, 杨吉波, 杨贺. 大兴安岭北段宝兴沟金矿床成矿流体特征及矿床成因[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1071-1084.
[6] 张锦让, 温汉捷, 邹志超. 滇西北兰坪盆地金满脉状铜矿床成矿流体特征及其成矿意义[J]. 吉林大学学报(地球科学版), 2017, 47(3): 706-718.
[7] 张艳, 韩润生, 魏平堂, 邱文龙. 云南会泽矿山厂铅锌矿床流体包裹体特征及成矿物理化学条件[J]. 吉林大学学报(地球科学版), 2017, 47(3): 719-733.
[8] 王力, 孙丽伟. 山东省寺庄金矿床成矿流体特征[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1697-1710.
[9] 王可勇, 付丽娟, 韦烈民, 王志高. 辽宁榛子沟铅锌矿床热液叠加成矿作用特征及成矿流体来源[J]. 吉林大学学报(地球科学版), 2016, 46(1): 80-90.
[10] 贾福聚, 燕永锋, 伍伟, 刘晓玮. 云南老君山锡多金属成矿区硫、铅、氢、氧同位素地球化学[J]. 吉林大学学报(地球科学版), 2016, 46(1): 105-118.
[11] 张志辉, 张达, 狄永军, 李兴俭, 阙朝阳, 马先平, 杜泽忠. 安徽铜陵焦冲金矿床成矿流体特征及成矿机制[J]. 吉林大学学报(地球科学版), 2015, 45(6): 1657-1666.
[12] 王承洋, 王可勇, 周向斌, 李文, 黄广环, 李剑锋, 张雪冰, 于琪. 内蒙古东山湾钨钼多金属矿床成矿流体地球化学特征及成因[J]. 吉林大学学报(地球科学版), 2015, 45(3): 759-771.
[13] 王力，潘忠翠，孙丽伟. 山东莱州新城金矿床流体包裹体[J]. 吉林大学学报(地球科学版), 2014, 44(4): 1166-1176.
[14] 熊索菲，姚书振，宫勇军，何谋春，祁冬梅，向鹏. 河南祁雨沟金矿临界-超临界包裹体特征及成矿流体演化[J]. 吉林大学学报(地球科学版), 2014, 44(1): 120-133.
[15] 宋明春，李三忠，伊丕厚，崔书学，徐军祥，吕古贤，宋英昕，姜洪利，周明岭，张丕建，黄太岭，刘长春，刘殿浩. 中国胶东焦家式金矿类型及其成矿理论[J]. 吉林大学学报(地球科学版), 2014, 44(1): 87-104.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
版权所有 © 《吉林大学学报(地球科学版)》编辑部
地址：长春市西民主大街938号(130026)　电话：+86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
本系统由北京玛格泰克科技发展有限公司设计开发