| 桦树沟铁铜矿床地质特征 |
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| 引用本文： | 徐卫东.桦树沟铁铜矿床地质特征[J].地质找矿论丛,2005,20(Z1):117-119. |
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| 作者姓名： | 徐卫东 |
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| 作者单位： | 中国冶金地质勘查工程总局,西北地质勘查院,西安,710061;中国地质大学,北京,100083 |
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| 摘 要： | 文章概述了桦树沟铁铜矿床主要地质特征及矿床成因信息资料,根据矿床勘探资料结合同行研究成果,探讨了矿床成因.认为矿床的多期、多阶段、多成因特征明显,区域地质找矿工作不能受"上铜下铁"模式的束缚.
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| 关 键 词： | 桦树沟铁铜矿床 地质特征 地球化学特征 甘肃省 |
| 文章编号： | 1001-1412(2005)S0-0117-03 |
| 修稿时间： | 2005年4月5日 |
THE COMPREHENSIVE GEOLOGICAL SIGNATURES AND REGIONAL GEOLOGICAL PROSPECTING OF HUASHUGOU Fe-Cu DEPOSIT |
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| XU Wei-dong.THE COMPREHENSIVE GEOLOGICAL SIGNATURES AND REGIONAL GEOLOGICAL PROSPECTING OF HUASHUGOU Fe-Cu DEPOSIT[J].Contributions to Geology and Mineral Resources Research,2005,20(Z1):117-119. |
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| Authors: | XU Wei-dong |
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| Abstract: | This Paper summarizes the main geological signatures and the origin information of Huashugou Fe-Cu deposit, and probes into the deposit origin by mathematical geological analysis, lithogeochemical information and integrated research of other geological signatures. It is characterized by multi-epoch, muliti-stage ore formation and multi-genesis. Regional oresearching should not be constrained by the top Cu-bottom Fe model. |
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| Keywords: | Huashugou Fe-Cu deposit geological signatures lithogeochemistry mathematical geological analysis Gunsu province |
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