| 西藏岗讲斑岩铜钼矿地质特征及找矿远景 |
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| 引用本文： | 张庆松,周维德. 西藏岗讲斑岩铜钼矿地质特征及找矿远景[J]. 地质找矿论丛, 2006, 21(Z1): 27-29 |
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| 作者姓名： | 张庆松 周维德 |
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| 作者单位： | 四川省冶金地质勘查院,成都,610051 |
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| 基金项目： | 中国地质调查局区域地质调查项目 |
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| 摘 要： | 岗讲斑岩型铜钼矿产于续迈单元含斑中粒角闪黑云二长花岗岩中,受断层带及附近节理、裂隙的控制,矿区有弱硅化、钾化、黄铁矿化、青磐岩化、泥化等蚀变;岗讲现已圈定矿体4个.矿区矿化范围大,有较大规模和较高强度的物化探异常,具有大型-超大型矿床的远景.对下步工作提出了较为合理可行的建议.
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| 关 键 词： | 岗讲铜钼矿 斑岩型矿床 找矿远景 西藏自治区 |
| 文章编号： | 1001-1412(2006)S0-0027-03 |
| 修稿时间： | 2006-07-10 |
GEOLOGICAL CHARACTERISTICS AND ORE POTENTIAL OF GANGJIANG PORPHYRY COPPER-MOLYBDENUM DEPOSIT, TIBET |
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| ZHANG Qing-song,ZHOU Wei-de. GEOLOGICAL CHARACTERISTICS AND ORE POTENTIAL OF GANGJIANG PORPHYRY COPPER-MOLYBDENUM DEPOSIT, TIBET[J]. Contributions to Geology and Mineral Resources Research, 2006, 21(Z1): 27-29 |
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| Authors: | ZHANG Qing-song ZHOU Wei-de |
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| Abstract: | Gangjiang porphyry Cu,Mo deposit occurs in the spotted medium-grain amphibole-biotite monzonitic granite and is controlled by fault and joints and fractures near the fault.In the working area weak silicification,potassium alteration,pyritization,propylitization,argillation etc.are developed.Wide spread mineralization and big and high intensity geophysical and geochemical anomalies indicate that the deposit is of potential for large-super-large Cu,Mo deposit and proposals for further exploration are put forword. |
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| Keywords: | Gangjiang porphyry Cu Mo deposit porphyry ore deposit ore potential Tibet |
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