马达加斯加金矿床成因及找矿标志研究
收稿日期: 2013-11-29
修回日期: 2014-02-17
网络出版日期: 2014-08-26
基金资助
中国博士后科学基金项目“马达加斯加Maevatanana金矿床成因研究”（编号：2013M541000）和中国地质调查局地质大调查项目“全球巨型成矿带找矿勘查方法技术研究”（编号：12120113102100）联合资助.
Research on Genesis and Prospecting Indicators of Gold Deposits in Madagascar
Received date: 2013-11-29
Revised date: 2014-02-17
Online published: 2014-08-26
杨喜安 , 刘善宝 , 赵宪东 . 马达加斯加金矿床成因及找矿标志研究[J]. 黄金科学技术, 2014 , 22(2) : 1 -6 . DOI: 10.3969/j.issn.1005-2518.2014.02.001
The gold deposit in the Madagascar is a classical quartz vein type gold deposit，the gold mineralization developed in the quartz vein and its wall rock.The gold deposit is intersected by major NNW trending shear zones and east-trending fracture sets，gold mineralization is associated with Pan-African orogeny.In the Pan-African orogeny，there are intensive tectonic-magmatic in Madagascar，results partial melting of the lower crust，a large amount of fluids and granitic magma are formed.In the process of the ascent of the fluids，mixed shallow-sourced meteoric fluid，the ore-forming fluids would have entered the favourable faults，resulting in mineralization.
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