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王嘉玮, 朱裕生. 2019. 界面成矿探讨[J]. 中国地质, 46(1): 77-86. doi: 10.12029/gc20190105
引用本文: 王嘉玮, 朱裕生. 2019. 界面成矿探讨[J]. 中国地质, 46(1): 77-86. doi: 10.12029/gc20190105
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WANG Jiawei, ZHU Yusheng. 2019. A discussion on marginal metallogenesis[J]. Geology in China, 46(1): 77-86. doi: 10.12029/gc20190105
Citation: WANG Jiawei, ZHU Yusheng. 2019. A discussion on marginal metallogenesis[J]. Geology in China, 46(1): 77-86. doi: 10.12029/gc20190105
shu

界面成矿探讨

  • 中国地质科学院矿产资源研究所, 北京 100037

  • 基金项目:
    中国地质调查局项目（DD20160101）资助
详细信息
    作者简介: 王嘉玮, 男, 1989年生, 硕士, 从事矿床地质学、区域成矿学、矿产资源潜力评价理论与实践研究; E-mail:wangjiawei0824@163.com
    通讯作者: 朱裕生, 男, 1937年生, 研究员, 主要从事区域成矿学、矿产勘查、矿产区划、矿产预测理论及方法、矿产资源潜力评价等方面的理论研究; E-mail:zhuyushengchy@163.com

  • 中图分类号: P612

A discussion on marginal metallogenesis

  • Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

  • Fund Project: Supported by China Geological Survey Program (No. DD20160101)
More Information
    Author Bio: WANG Jiawei, male, born in 1989, master, majors in mineral deposits and engages in research on theory and practice of mineral resource potential assessment. E-mail:wangjiawei0824@163.com .
    Corresponding author: ZHU Yusheng, male, born in 1937, majors in regional metallogenesis, engages in research on theory of mineral resource potential assessment. E-mail: zhuyushengchy@163.com

    摘要

  • “地质界面”是地壳内各类地质单元的边界，它明确了地质体之间的相互关系，通常也是形成矿床的有利地质空间和载体；“成矿界面”是指地质界面上发生成矿作用的地质记录，记载有成矿作用发生的“地质界面”称它为“成矿界面”；讨论“地质界面”上发生成矿作用过程、成矿物质富集条件和矿床形成后保存过程的这一系列完整内容的成矿学理论，称为“界面成矿”理论。在前人研究基础上，匹配相应成矿作用种类，“成矿界面”可以概括分成9个成矿界面组；每类“成矿界面”上发生的成矿作用，都标定了矿床形成的地质位置，均对找矿有指示性意义；界面成矿理论是矿产预测和矿床勘查成矿学的重要依据，是总结成矿规律的基本内容之一，并且可以作为支撑境内外实施科学找矿的有效理论依据。

    "Geological interface" is the boundary of various geological units in the earth's crust. It clarifies the contact relationship between geological bodies, and usually also a geological space where the deposit is formed."Metallogenic interface" refers to the place where mineralization occurs and geological interface with the deposit."Marginal metallogenesis" clarifies the occurrence of mineralization at the metallogenic interface and its evolution process, ore-forming material enrichment and post-mineralization preservation process. According to the differences in geological and metallogenic processes, the metallogenic interface can be divided into 9 groups. Metallogenic interfaces are the most easily recognizable and direct indications for prospecting, and constitute one of the theoretical bases of scientific prospecting, and summarize the law of mineralization.

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  • 图 1  河南余冲金矿区同构造断裂系统-成矿流体渗滤成矿作用成矿界面图

    Figure 1. 

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    图 2  构造运动应力-改造沉积间断面界面成矿作用图示

    Figure 2. 

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    图 3  黄山东矿床28号勘探线剖面

    Figure 3. 

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    图 4  吉尔吉斯坦海达尔坦汞锑矿床成矿界面图

    Figure 4. 

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    图 5  白面山锡锌硫化物矿床024号勘探线剖面界面成矿图

    Figure 5. 

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    图 6  攀枝花钒钛磁铁矿矿区基性岩和矿床（体）赋存位置关系略图

    Figure 6. 

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    图 7  攀枝花钒钛磁铁矿矿区铁镁质岩浆侵入体岩相分带和矿体分布地质空间关系图

    Figure 7. 

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    图 8  华北溶洼型铝土矿成矿界面示意图

    Figure 8. 

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    表 1  成矿界面组分类

    Table 1.  Division of metallogenic interface group

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收稿日期:  2018-04-18
修回日期:  2019-01-03
刊出日期:  2019-02-25

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