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地球科学进展  2001, Vol. 16 Issue (4): 514-519    DOI: 10.11867/j.issn.1001-8166.2001.04.0514
综述与评述     
斑岩铜矿研究的若干进展
王奖臻1,2,李朝阳1,胡瑞忠1
1.中国科学院地球化学研究所矿床地球化学开放研究实验室,贵州 贵阳 550002;
2.成都理工学院,四川 成都 610059
RESEARCH PROGRESS IN PORPHYRY COPPER DEPOSIT
WANG Jiangzhen1,2,LI Chaoyang1,HU Ruizhong1
1. Open Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, CAS, Guiyang 550002,China;
2. Chengdu University of Technology, Chengdu 610059,China
 全文: PDF(1204 KB)  
摘要:

综述了近年来斑岩铜矿研究领域取得的最新成果。包括6个方面:①斑岩铜矿与岩浆的氧化状态有关,只有氧化型岩浆才能形成斑岩铜矿,并提出了确定岩浆氧化状态的新标志;②岩浆中硫和氯的含量、存在状态、溶解度等对成矿有重要控制作用;③岩浆能否较早达到水过饱和状态,并发生流体相的出溶是成矿的另一个控制因素;④俯冲板片释放出的流体对上覆楔形地幔的交代作用是形成含矿岩浆的重要环节;④岩浆混合或底侵作用可能在某些斑岩铜矿成矿中起到了重要作用;⑤提出了一些新的成矿及找矿标志,如早期磁铁矿蚀变相。

关键词: 斑岩铜矿成矿作用矿化剂研究进展    
Abstract:

The progress in research on porphyry copper deposit is viewed, including the following five aspects: (1) It has been proved that porphyry copper deposit is related to oxidized-type granite magma. And some new symbol which can be used to determine the redox state of magmas have been established. (2) The contents and solubility of sulfur and chlorine in magma are very important to the mineralization of porphyry copper deposit. (3) It has been illustrated that the earlier reached the oversaturation of water during magmatism, the more advantageous for the mineralizatuon. (4) Mantale metasomatism and magma mixing plays an important role in the origin of the magma which relate to the deposit. (5) Some new kinds of alteration in the deposit, such as magnetite alteration facies and Na-Ca alteration, have been discovered and studied.

Key words: Porphyry copper deposit    Mineralization    Research progress
收稿日期: 2000-07-26 出版日期: 2001-08-01
:  P618.41  
基金资助:

博士后基金项目“氧化性岩浆作用——斑岩铜矿形成的关键因素”;国家杰出青年基金项目“热液矿床矿化剂地球化学”(编号:49925309)资助.

通讯作者: 王奖臻(1959-),男,河北人,副教授,主要从事矿床地质研究.     E-mail: lzq@cdit.edu.cn
作者简介: 王奖臻(1959-),男,河北人,副教授,主要从事矿床地质研究. E-mail:lzq@cdit.edu.cn
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引用本文:

王奖臻,李朝阳,胡瑞忠. 斑岩铜矿研究的若干进展[J]. 地球科学进展, 2001, 16(4): 514-519.

WANG Jiangzhen, LI Chaoyang,HU Ruizhong. RESEARCH PROGRESS IN PORPHYRY COPPER DEPOSIT. Advances in Earth Science, 2001, 16(4): 514-519.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.2001.04.0514        http://www.adearth.ac.cn/CN/Y2001/V16/I4/514

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