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地球科学进展  1995, Vol. 10 Issue (1): 40-46    DOI: 10.11867/j.issn.1001-8166.1995.01.0040
干旱气候变化与可持续发展     
斑岩铜矿床研究综述
高合明
中国科学院地球化学研究所  贵阳  550002
A SUMMARY OF RESEARCHES ON PORPHYRY COPPER DEPOSITS
Gao Heming
Institute of Geochemistry, Chinese Academy of Sciences,Guiyang  550002
 全文: PDF(342 KB)  
摘要:

综述了板块构造、大地构造单元、区域构造、深大断裂以及地球深部热点与斑岩铜矿床形成关系的研究成果,系统介绍了斑岩铜矿床蚀变矿化分带特征、蚀变矿化物理化学条件、蚀变矿化的热力学研究、斑岩铜矿床中脉体的产状和分布特征以及成因观点,总结了斑岩铜矿床成矿物质来源与矿床成因模式,最后指出了斑岩铜矿床将来应该注意的研究方向。

关键词: 斑岩铜矿床蚀变矿化成因模式脉体    
Abstract:

The main achievements of the genetic relationships between porphyry copper deposits and plate tectonics, tectonic unit, regional structure, long and deep regional fracture and hot point in the mantle are summarized. The most important characteristics of zoning of alteration and mineralization and the primary features of distribution and dips of veins in porphyry copper deposits as well as genetic views for the veins are synthesized. The significant investigations about physico-chemical coditions of rock-forming and ore-forming processes, the sources of ore-forming matter, the major genetic patterns for the deposits and some important aspects which should be studied in detail by complex sciences are show in this article.

Key words: Vein    Genetic pattern.    Porphyry copper deposit    Alteration    Mineralization
收稿日期: 1994-02-01 出版日期: 1995-02-01
基金资助:

国家自然科学基金项目“斑岩铜矿床成矿作用的构造地球化学动力学研究”(编号:49303042)资助.

通讯作者: 高合明   
作者简介: 高合明
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引用本文:

高合明. 斑岩铜矿床研究综述[J]. 地球科学进展, 1995, 10(1): 40-46.

Gao Heming. A SUMMARY OF RESEARCHES ON PORPHYRY COPPER DEPOSITS. Advances in Earth Science, 1995, 10(1): 40-46.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.1995.01.0040        http://www.adearth.ac.cn/CN/Y1995/V10/I1/40

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