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物探与化探  2019, Vol. 43 Issue (5): 925-931    DOI: 10.11720/wtyht.2019.0198
  特约稿件 本期目录 | 过刊浏览 | 高级检索 |
关于胶西北金矿成矿地球化学机制的思考
马生明1, 朱立新2, 张亮亮1,3, 王建1
1. 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
2. 中国地质调查局,北京 100037
3. 山东省第六地质矿产勘查院,山东 威海 264200
Thoughts on the geochemical mechanism of gold mineralization in the northwest Jiaodong gold province
Sheng-Ming MA1, Li-Xin ZHU2, Liang-Liang ZHANG1,3, Jian WANG1
1. Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Science, Langfang 065000, China
2. China Geological Survey, Beijing 100037, China
3. No. 6 Geology and Mineral Resources Institute, Weihai 264200,China
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摘要 

胶西北地区海域、焦家和大尹格庄金矿床钻孔岩石测量结果显示,这些金成矿系统中存在着矿化剂元素S、常量元素Na2O以及成矿元素Au等多属性地球化学异常,递进地指示了金矿的成矿条件和成矿前景,为深部金矿勘查提供了地球化学依据。在对这些异常体系形成机理深入认知的基础上,提出了胶西北金矿成矿的地球化学机制,概括为矿源、富硫、重组、水火、耦合和向心等六个方面。综合相关40余个试验区研究成果,关于胶西北金矿成矿地球化学机制的认识,在其他地区包括金矿在内的热液成因金属矿床均成立,是矿床地球化学勘查应用理论及方法的进步和发展。

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关键词 胶西北金成矿地球化学机制    
Abstract

The borehole rock measurement of Jiaojia, Haiyu and Dayingezhuang gold deposits in northwest Jiaodong gold province shows that the multi-attribute geochemical anomaly system, which consists of mineralizer element S, major element Na2O and ore-forming element Au, progressively indicates the gold ore-forming conditions, metallogenic prospect and geochemical basis for deep prospecting. Through a study of formation mechanism of multi-attribute geochemical anomaly, this paper puts forward the geochemical mechanism of gold mineralization in northwest Jiaotong gold province, which can be summarized as ore source, sulfur enrichment, recombination, fluid and heat, coupling and centripetal. Based on the study of 40 experimental areas, the authors hold that the ore-forming geochemical mechanism of the Jiaojia-type gold deposits and the other hydrothermal metallic mineral deposits is the innovation and development of theory and method on the exploration geochemistry application.

Key wordsnorthwest Jiaodong    gold mineralization    geochemical mechanism
收稿日期: 2019-04-08      出版日期: 2019-10-25
:  P632  
基金资助:国家科技支撑计划项目(2014BAB05B00)
作者简介: 马生明(1963-),男,博士,教授级高级工程师,主要从事勘查地球化学理论方法研究及矿产地质、生态地质调查工作。Email: mashengming@igge.cn
引用本文:   
马生明, 朱立新, 张亮亮, 王建. 关于胶西北金矿成矿地球化学机制的思考[J]. 物探与化探, 2019, 43(5): 925-931.
Sheng-Ming MA, Li-Xin ZHU, Liang-Liang ZHANG, Jian WANG. Thoughts on the geochemical mechanism of gold mineralization in the northwest Jiaodong gold province. Geophysical and Geochemical Exploration, 2019, 43(5): 925-931.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2019.0198      或      https://www.wutanyuhuatan.com/CN/Y2019/V43/I5/925
Fig.1  胶西北地区地质及试验区位置简图
Fig.2  三仓、龙莱和招平断裂带空间分布示意
Fig.3  焦家试验区构造蚀变带上盘(a)、下盘(b)岩石结构构造图示
Fig.4  焦家试验区构造蚀变带上盘/下盘花岗岩REE配分模式图示
Fig.5  焦家试验区构造蚀变带/下盘花岗岩REE配分模式图示
Fig.6  焦家试验区128勘探线钻孔岩石测量Au异常图示
Fig.7  焦家试验区128勘探线钻孔岩石测量S异常图示
Fig.8  焦家试验区128勘探线钻孔岩石测量Na2O负异常图示
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