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  • CN 62-1112/TF 
  • ISSN 1005-2518 
  • 创刊于1988年
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矿产勘查与资源评价

地震与成矿过程研究综述

  • 梁光河
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  • 1.中国科学院矿产资源研究重点实验室,北京   100029;
    2.中国科学院地质与地球物理研究所,北京   100029
梁光河(1965-),男,河南新野人,博士,副研究员,从事地震、大地构造及矿产资源研究工作。lgh@mail.iggcas.ac.cn

收稿日期: 2016-08-05

  修回日期: 2016-10-09

  网络出版日期: 2017-01-22

基金资助

中国科学院深部资源探测核心装备研发专项“金属矿地震探测系统”(编号:ZDYZ2012-1-06)资助

Summary of Research on Earthquake and Metallogenic Process

  • LIANG Guanghe
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  • 1.Key Laboratory of Mineral Resources Research,Chinese Academy of Sciences,Beijing   100029,China;
    2.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing   100029,China

Received date: 2016-08-05

  Revised date: 2016-10-09

  Online published: 2017-01-22

摘要

天然地震主要包括构造地震和火山地震,越来越多的证据表明构造地震是一种隐爆过程,如同火山爆发,其与成矿密切相关。地震过程是一种地下超临界流体的相变过程,通常表现为流体的退相爆炸。隐爆角砾岩型、斑岩型及浅成热液型矿床的成因与地震密切相关。汶川地震后通过开展地球物理探测发现地下很可能存在中间岩浆房和原始岩浆房,地震过程中的侵位使得浅部富集了P、S、Fe、Mn等元素。诸多研究和实例说明构造地震是一种由断裂运动激发引起的地下隐爆和成矿过程,研究震裂的特征以及伴生蚀变矿物的物性特征对找矿具有一定的指导意义。

本文引用格式

梁光河 . 地震与成矿过程研究综述[J]. 黄金科学技术, 2016 , 24(6) : 8 -14 . DOI: 10.11872/j.issn.1005-2518.2016.06.008

Abstract

 Earthquakes mainly include tectonic and volcanic earthquakes.More and more evidences show that the tectonic earthquake is a kind of hidden explosion process.They usually have close relation with metallogenic process as volcanic eruption.Earthquake process is a phase transition process of subsurface supercritical fluid,which is usually shown as dephasing explosion.The origin of the cryptoexplosion breccias type deposit,the porphyry type deposit and the shallow hydrothermal type deposit is closely related to the earthquake.Geophysical exploration after the Wenchuan earthquake found that there likely exist original magma chambers and middle magma chamber in the deep,the invasion in this earthquake process makes the shallow enrichment of phosphorus,sulfur,iron,manganese and other elements.Many studies and examples illustrate that the earthquake is an underground hidden explosion and ore-forming process triggered by fault motion.The research on  the characteristics of the seismic fracture and the physical characteristics of the associated alteration minerals are of guiding significance for the exploration of mineral deposits.

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