吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (4): 1104-1118.doi: 10.13278/j.cnki.jjuese.201704111

• 地质与资源 • 上一篇    下一篇

治岭头金矿围岩蚀变特征及其意义

郝立波1, 吴超2,3, 赵新运1, 赵玉岩1, 陆继龙1, 魏俏巧1   

  1. 1. 吉林大学地球探测科学与技术学院, 长春 130026;
    2. 国土资源部地球化学探测技术重点实验室, 河北 廊坊 065000;
    3. 中国地质科学院地球物理地球化学勘查研究所, 河北 廊坊 065000
  • 收稿日期:2016-11-25 出版日期:2017-07-26 发布日期:2017-07-26
  • 通讯作者: 赵新运(1988),男,讲师,博士,主要从事地球化学研究工作,E-mail:zhaoxy15@jlu.edu.cn E-mail:zhaoxy15@jlu.edu.cn
  • 作者简介:郝立波(1961),男,教授,博士生导师,主要从事地球化学研究工作,E-mail:haolb@jlu.edu.cn
  • 基金资助:
    中国地质调查局项目（20089941）；中央级公益性科研院所基本科研业务费专项（AS2016P02）

Characteristics of Wall Rock Alteration of Zhilingtou Gold Deposit and Its Significance

Hao Libo1, Wu Chao2,3, Zhao Xinyun1, Zhao Yuyan1, Lu Jilong1, Wei Qiaoqiao1   

  1. 1. College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China;
    2. Key Laboratory of Geochemical Exploration, Ministry of Land and Resources, Langfang 065000, Hebei, China;
    3. Institute of Geophysical and Geochemical Exploration, CAGS, Langfang 065000, Hebei, China
  • Received:2016-11-25 Online:2017-07-26 Published:2017-07-26
  • Supported by:
    Supported by Project of the China Geological Survey (20089941) and Basal Research Fund of Central Public Welfare Scientific Institution(AS2016P02)

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摘要： 治岭头金矿位于浙江省遂昌县，是我国东南沿海的一座大型金矿床。该矿床围岩蚀变发育，类型有硅化、绢云母化、绿泥石化、黄铁矿化、方解石化和菱锰矿化。从矿体到围岩可以划分为4个蚀变带：强硅化带、弱硅化-黄铁绢英岩化带、绢云母化带和绿泥石化带。沿矿体走向，蚀变强度整体上呈波动性变化，与矿体呈透镜状产出特征一致。硅化、黄铁矿化、菱锰矿化与金矿化关系最密切，而且这些蚀变具有相似的变化趋势。绢云母化和绿泥石化与硅化的变化趋势不同，且与矿化关系不密切。另外，矿区还发育方解石化，且强度较弱。金矿化及围岩蚀变均发育在古元古界八都群变质岩中，未进入上覆中生代火山岩盖层，证明治岭头金矿成矿作用与中生代火山活动无关。定量计算结果显示：蚀变过程中Al2O3、TiO2、P2O5为惰性组分；SiO2、CaO、MnO、Au、Ag、Cu、Pb、Zn等为明显带入组分；Fe2O3、FeO、MgO、K2O、Na2O、Ba、Sr等为明显带出组分。根据围岩蚀变和稳定同位素分析，推断治岭头金矿原始成矿热液流体应是富含Si、Ca、Mn、Au、Ag、Cu、Pb、Zn等组分的岩浆热液，后期有大气降水的加入。

关键词: 治岭头金矿, 围岩蚀变, 蚀变分带, 质量迁移

Abstract: Located in Suichang, Zhejiang Province, Zhilingtou deposit is a large gold deposit on the southeastern coast of China. Its wall rock alterations are widespread in Zhilingtou gold deposit, such as silicification, sericitization, chloritization, pyritization, calcitization and siderite manganese mineralization. From ore body to wall rock, the alteration zone can be divided into quartz-rich, beresitization with quartz, sericite, and chlorite zones. In general, the alteration degree fluctuates with the distance to ore bodies, and forms a shape of lens just as the shape of an ore body surrounded. Gold mineralization is associated with quartz, pyrite, and rhodochrosite alterations. Quartz alteration, pyrite alteration, and rhodochrosite alteration degrees have a similar changing trend; while the sercite and chlorite alteration trend is different. In addition, the deposit develops a low degree of calcite alteration. Both gold mineralization and wall rock alteration occurred in the Paleoproterozoic metamorphic rocks of Badu Group, and did not enter overlying Mesozoic volcanic rocks, which indicates that the formation of the deposit has no relation with the Mesozoic volcanic activities. The elemental quantitative analysis showed that Al2O3, TiO2 and P2O5 were inactive components, SiO2, CaO, MnO, Au, Ag, Cu, Pb, Zn, etc. were gathered,and Fe2O3, FeO, MgO, K2O, Na2O, Ba, Sr, etc. were lost from the wall rocks in alteration process. According to the alteration features and stable isotope analysis, we conclude that the primitive hydrothermal ore-forming fluids of the deposit were mainly of magmatic water with enrichment in Si, Ca, Mn, Au, Ag, Cu, Pb, Zn, etc., and some meteoric water were added to the fluids in ore forming process.

Key words: Zhilingtou gold deposit, wall rock alteration, alteration zone, mass transport

中图分类号: 

  • P618.51
[1] 陈天虎. 浙江治岭头金矿石英热释光研究[J]. 安徽地质,2000, 10(1): 29-34. Chen Tianhu, Study on Thermoluminescence of Quartz in the Gold Deposit at Zhilingtou, Zhejiang Province[J]. Geology of Anhui, 2000, 10(1): 29-34.
[2] 张丕富,吴锡生,梁乃杰,等. 浙江治岭头金银矿床成矿成晕模式[J]. 地质评论,1991, 37(5): 429-436. Zhang Pifu, Wu Xisheng, Liang Naijie, et al. A Model of Ore and Halo Formation for the Zhilingtou Gold-Silver Deposit, Zhejiang[J].Geological Review, 1991, 37(5): 429-436.
[3] 李升先. 对遂昌治岭头金矿的几点看法[J]. 浙江地质,1998, 14(2): 29-35. Li Shengxian. Opinions on the Zhilingtou Gold Mine of Suichang County[J]. Geology of Zhejiang, 1998, 14(2): 29-35.
[4] 梁子豪,朱清涛,韩梦合,等. 浙江治岭头金银矿床成矿条件研究[J]. 地质评论,1985, 31(4): 330-340. Liang Zihao, Zhu Qingtao, Han Menghe, et al. Metallogenic Conditions of the Zhilingtou Gold-Silver Deposit in Zhejiang Province[J]. Geological Review, 1985, 31(4): 330-340.
[5] 章传玲,姚书振,王苹,等. 浙江遂昌治岭头金银矿床硅同位素研究[J]. 地球科学:中国地质大学学报,1998, 23(5): 499-501. Zhang Chuanling, Yao Shuzhen, Wang Ping, et al. Study on the Silicon Isotope of Zhilingtou Gold-Silver Deposit in Suichang, Zhejiang Province[J]. Earth Science: Journal of China University of Geosciences, 1998, 23(5): 499-501.
[6] 邱小平,华杰雄,钱建民,等. 浙江省遂昌县治岭头金矿成矿构造特征[C]//安徽省地质学会. 2007年华东六省一市地学科技论坛论文集. 合肥:合肥工业大学出版社,2007: 204-209. Qiu Xiaoping, Hua Jiexiong, Qian Jianmin, et al. Metallogenic Structure Characteristics of Zhilingtou Gold Mine of Suichang County, Zhejiang Province[C]//Anhui Province Geological Society. Workshop on Geological Science and Technology in East China. Hefei: Hefei University of Technology Press, 2007: 204-209.
[7] 梅建明. 浙江遂昌治岭头金矿床黄铁矿的化学成分标型研究[J]. 现代地质,2000, 14(1): 51-55. Mei Jianming. Chemical Typomorphic Characteristic of Pyrites from Zhilingtou Gold Deposit, Suichang, Zhejiang[J]. Geoscience, 2000, 14(1): 51-55.
[8] 冀桂清,邵军.论治岭头金银矿床的成因[J]. 贵金属地质,1998, 7(4): 250-257. Ji Guiqing, Shao Jun. Origin of Zhilingtou Gold-Silver Deposit in Zhejiang Province[J]. Journal of Precious Metallic Geology, 1998, 7(4): 250-257.
[9] 胡雄健,陈程华,李春忠. 浙江治岭头金矿床成矿条件探讨[J]. 贵金属地质,1993, 2(3): 223-232. Hu Xiongjian, Chen Chenghua, Li Chunzhong. On Metallogenic Factors of Zhilingtou Gold Deposit in Zhejiang Province[J]. Journal of Precious Metallic Geology, 1993, 2(3): 223-232.
[10] 周俊法,钱建民. 治岭头金银矿床的形成时代[J]. 浙江地质,1996, 12(1): 60-67. Zhou Junfa, Qian Jianmin. The Metallogenic Epoch of Zhilingtou Gold-Silver Deposit[J]. Geology of Zhejiang, 1996, 12(1): 60-67.
[11] 赵超,倪培,王国光,等. 浙西南治岭头斑岩钼矿体流体包裹体研究[J]. 高校地质学报,2014, 3(20): 38-49. Zhao Chao, Ni Pei, Wang Guoguang, et al. The Fluid Inclusions Study on Zhilingtou Molybdenum Deposit in Southwest Zhejiang Province[J]. Geological Journal of China Universities, 2014, 3(20): 38-49.
[12] 钱建民,濮为民,钟增球,等. 浙江遂昌治岭头筒状铅锌矿体地质特征及成因[J]. 大地构造与成矿学,2010, 34(1): 63-70. Qian Jianmin, Pu Weimin, Zhong Zengqiu, et al. Geologic Characteristics and Genesis of the Zhilingtou Cylindrical Lead-Zinc Deposit in Suichang Zhejiang[J]. Geotectonica et Metallogenia, 2010, 34(1): 63-70.
[13] 郑明华,刘建明. 论浙江治岭头金银矿床的成矿物质来源[J]. 矿床地质,1986, 5(1): 39-52. Zheng Minghua, Liu Jianming. Material Sources of the Zhilingtou Gold-Silver Ore Deposit in Zhejiang Province[J]. Mineral Deposits, 1986, 5(1): 39-52.
[14] 濮为民. 治岭头地区金银矿地质特征及矿床成因[J]. 有色金属(矿山部分),2009, 61(3): 24-28. Pu Weimin. Geological Characteristics and Genesis of Zhilingtou Gold-Silver Deposit[J]. Nonferrous Metals (Mine Section), 2009, 61(3): 24-28.
[15] Grant J A. The Isocon Diagram:A Simple Solution to Gresens' Eqution for Metasomatic Alteration[J]. Economic Geology, 1986, 81: 1976-1982.
[16] Baumgartner L P, Olsen S N. A Least-Squares Approach to Mass Transport Calculations Using the Isocon Method[J]. Economic Geology, 1995, 100: 1261-1270.
[17] 高斌,马东升.围岩蚀变过程中地球化学组份质量迁移计算:以湖南沃溪Au-Sb-W矿床为例[J]. 地质找矿论丛,1999, 14(2): 23-29. Gao Bin, Ma Dongsheng. Identifying the Immobile Elements and Evaluating Mass Transport in the Geochemical Process of the Wall-Rock Alteration: Applied to the Woxi Gold-Antimony-Wolfram Deposit in Hunan Province, China[J]. Contributions to Geology and Mineral Resources Research, 1999, 14(2): 23-29.
[18] 卢新哲. 遂昌治岭头金矿矿床地质特征和成矿作用研究[D]. 合肥:合肥工业大学,2014: 55-56. Lu Xinzhe. Study on Suichang Zhilingtou Deposit Geological Feature and Mineralization[D]. Hefei: Hefei University of Technology, 2014: 55-56.
[19] 陈天虎,林文通. 浙江治岭头金矿床成因研究[J]. 合肥工业大学学报,1994, 17(1): 187-192. Chen Tianhu, Lin Wentong.Minerogenic Mechanism of Zhilingtou Gold Deposit in Zhejiang Province[J]. Journal of Hefei University of Technology, 1994, 17(1): 187-192.
[20] 吴香尧.浙江治岭头金矿蚀变作用过程金的活化运移与富集[J]. 成都地质学院学报,1989, 16(1): 1-8. Wu Xiangyao. Gold Mobilization, Migration and Enrichment in Alteration Process of Zhilingtou Deposit Zhejiang, China[J]. Journal of Chengdu College of Geology, 1989, 16(1): 1-8.
[21] 郑明华,刘建明.浙江治岭头金-银矿床形成的物理化学条件及成矿过程分析[J]. 地质学报,1987(3): 253-266. Zheng Minghua, Liu Jianming. Physico-Chemical Conditions and Ore-Forming Process of the Zhilingtou Gold-Silver Deposit, Zhejiang, Chian[J]. Acta Geologica Sinica, 1987(3): 253-266.
[22] 郑明华,刘建明.论浙江治岭头金-银矿床的成矿条件[J].成都地质学院学报,1986, 13(2): 16-29. Zheng Minghua, Liu Jianming. On Ore-Forming Conditions of the Zhilingtou Gold-Silver Ore Deposit, Zhejiang Province[J]. Journal of Chengdu College of Geology, 1986, 13(2): 16-29.
[23] 曹晓峰,Mohamed Lamine Salifou Sanogo, 吕新彪,等. 甘肃枣子沟金矿床成矿过程分析:来自矿床地质特征、金的赋存状态及稳定同位素证据[J]. 吉林大学学报(地球科学报),2012, 42(4): 1039-1054. Cao Xiaofeng, Mohamed Lamine Salifou Sanogo, Lü Xinbiao, et al. Ore-Forming Process of the Zaozigou Gold Deposit: Constraints from Geological Characteristics, Gold Occurrence and Stable Isotope Compositions [J]. Journal of Jilin University (Earth Science Edition), 2012, 42(4): 1039-1054.
[24] 胡受奚,叶瑛,方长泉. 交代蚀变岩岩石学及其找矿意义[M]. 北京:地质出版社,2004: 63-64. Hu Shouxi, Ye Ying, Fang Changquan. Petrology of Metasomatically Altered Rocks and Its Significance in Prospecting[M]. Beijing: Geological Press, 2004: 63-64.
[25] 吴超. 浙江省治岭头金矿围岩蚀变特征及意义[D]. 长春:吉林大学,2016. Wu Chao.Characteristics of Wall Rock Alteration and Its Significance of Zhilingtou Gold Deposit in Zhejiang Province[D]. Changchun: Jilin University, 2016.
[26] 郑人来,王华田,韩梦合,等. 浙东南(陈蔡—遂昌隆起)金矿成矿规律及成矿预测[R]. 杭州:浙江省地质矿产研究所,1989. Zheng Renlai, Wang Huatian, Han Menghe, et al.Metallogenic Regularity and Prediction to Gold Deposits in Southeast Zhejiang Province (Chencai-Suichang Swell) [R]. Hangzhou: Zhejiang Institute of Geology and Mineral Resources, 1989.
[27] 华杰雄,陈少华,毛伟雄,等. 治岭头金银矿床控矿构造因素及成矿模式[J]. 黄金科学技术,2000, 8(4): 27-34. Hua Jiexiong, Chen Shaohua, Mao Weixiong, et al. Structural Controls of Mineral Localization and Mineral Deposit model of Zhilingtou Gold-Silver Deposit[J]. Gold Science and Technology, 2000, 8(4): 27-34.
[28] 钱建民,钟增球,楼新涛,等. 浙江治岭头矿田地球化学特征的研究[J]. 金属矿山,2008(6): 82-93. Qian Jianmin, Zhong Zengqiu, Lou Xintao, et al. Study on Geochemical Characteristics of Zhilingtou Orefield in Zhejiang[J]. Metal Mine, 2008(6): 82-93.
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