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津巴布韦卢比(Ruby)矿床——南部非洲一典型的BIF型金矿床

津巴布韦卢比(Ruby)矿床——南部非洲一典型的BIF型金矿床

ISSN:1674-7801
2017年第8卷第1期
境外勘查
江伟华1,卿芸2,胡晓丽3,刘京3 JIANG Wei-hua1, QING Yun2, HU Xiao-li3, LIU Jing3
(1. 中国非金属矿工业协会,北京 100831;2. 中国冶金地质总局矿产资源研究院,北京 100025;3. 中矿资源勘探股份有限公司,北京 100089) (1. China Non-Metallic Minerals Industry Association, Beijing 100831;2. Institute of Mineral Resources Research, China Metallurgical Geology Bureau, Beijing 100025;3. Sinomine Resource Exploration Co., Ltd., Beijing 100089)

卢比金矿床位于津巴布韦克拉通中南部的马斯温戈绿岩带中,金矿体主要赋存在条带状含铁建造中的硫化物相、碳酸盐相中,成矿作用与火山喷发—沉积作用密切相关,为南部非洲一典型的BIF型金矿床。

The Ruby gold deposit is located at the Masvingo greenstone belt, south-central part of Zimbabwe craton. The ore bodies are mainly hosted in sulfide phase and carbonate phase of the banded iron formation, which are closely related to volcanic eruption and sedimental deposition process. The Ruby gold deposit is a typical BIF-hosted gold deposite in southern Africa.

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ISSN:1674-7801
2017年第8卷第1期
境外勘查

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