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马来西亚斯里加亚铁矿床地质特征及成因探讨
引用本文:祝明金,练兵,田亚洲,亢庚.马来西亚斯里加亚铁矿床地质特征及成因探讨[J].贵州地质,2011,28(3):206-210,236.
作者姓名:祝明金  练兵  田亚洲  亢庚
作者单位:1. 贵州大学资源与环境工程学院,贵州贵阳,550003
2. 中国铝业贵州分公司,贵州贵阳,550058
基金项目:作者同贵州大学资源与环境工程学院张竹如教授赴马来西亚对斯里加亚铁矿勘查的成果;在成文过程中张竹如教授给予了精心指导与帮助;同时也得了到贵州大学资源与环境工程学院聂爱国教授指导;在此深表感谢!
摘    要:本文阐明了马来西亚斯里加亚铁矿床的大地构造位置、区域地质、矿区地质,并结合原生矿体和氧化矿体的特征对该矿床的成因进行了分析,氧化矿主要为原生矿风化残积及部分坡积成因,原生矿体产于隐伏的燕山期花岗闪长岩外接触带,其围岩具典型的矽卡岩矿物组合,该矿床为矽卡岩型铁矿床。

关 键 词:铁矿  矿床特征  成因探讨  马来西亚斯里加亚

Geologic Character and Genesis of Srijaya Iron Deposit in Malaysia
ZHU Ming-jin,LIAN Bing,TIAN Ya-zhou,KANG Geng.Geologic Character and Genesis of Srijaya Iron Deposit in Malaysia[J].Guizhou Geology,2011,28(3):206-210,236.
Authors:ZHU Ming-jin  LIAN Bing  TIAN Ya-zhou  KANG Geng
Institution:ZHU Ming-jin1,LIAN Bing2,TIAN Ya-zhou1,KANG Geng1(1.Resource and Environment School of Guizhou University,Guiyang 550003,Guizhou,China,2.HALCO Guizhou Branch,Guiyang 550058,China)
Abstract:In this paper,the tectonic location,regional geology and mine geology are narrated,the genesis of this deposit is studied according to the characters of primary ore body and oxide ore body.The oxide ore is formed by primary ore weathering sedentary and partly slop wash.Primary ore body occurred in the hidden outer contact zone of granodiorite in Yanshan period,its wall rock is typical skarn mineral association and the deposit is skarn iron deposit.
Keywords:iron ore  deposit character  genesis  Srijiya
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