| 云南金平太平桥铁矿矿床地质及远景预测 |
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| 引用本文： | 孙云堂,陈斌.云南金平太平桥铁矿矿床地质及远景预测[J].云南地质,2012(2):208-210. |
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| 作者姓名： | 孙云堂 陈斌 |
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| 作者单位： | 云南省有色地质局312队 |
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| 摘 要： | 受红河右旋走滑深大断裂构造控制,铁矿床主要赋存于华力西期侵入基性-超基性岩杂岩体内,成矿专属性明显,矿床属晚期岩浆结晶分异型磁铁矿矿床。
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| 关 键 词： | 岩体控矿 基性分异体 磁铁矿 外围找矿远景 云南金平太平桥 |
THE GEOLOGY AND POTENTIALITY PROGNOSIS OF TAIPINGQIAO FE DEPOSIT OF JINPING,YUNNAN |
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| SUN Yun-tang,CHEN Bin.THE GEOLOGY AND POTENTIALITY PROGNOSIS OF TAIPINGQIAO FE DEPOSIT OF JINPING,YUNNAN[J].Yunnan Geology,2012(2):208-210. |
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| Authors: | SUN Yun-tang CHEN Bin |
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| Affiliation: | g (geological Team 312,Yunnan Bureau of Nonferrous Geology,Annining 650300) |
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| Abstract: | The Fe ore deposit is controlled mainly by Honghe right lateral strike slipfault.It is in the basic-ultrabasic complex of Variscan intrusion,with the evident metallogenetic specialization.It belongs to the magnetite deposit of late magmatic crystal differentiate type. |
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| Keywords: | Ore Control of Rock Body Basic Differentiate Magnetite Surrounding Prospecting Potentiality Taipingqiao Jinping Yunnan |
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