| 浙江青田石平川钼矿控矿条件分析 |
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| 引用本文： | 董良.浙江青田石平川钼矿控矿条件分析[J].云南地质,2010,29(4):431-433. |
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| 作者姓名： | 董良 |
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| 作者单位： | 浙江省第十一地质大队,浙江温州325000 |
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| 摘 要： | 石平川钼矿由燕山晚期第四次侵入碱性长石花岗岩体提供物源和热动力,火山机构、断裂和西山头组第二岩性段为成矿提供了导矿通道和容矿场所。
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| 关 键 词： | 蚀变凝灰岩型 细脉条带辉钼矿 火山机构控矿 晚燕山期花岗岩 浙江青田石平川 |
AN ANALYSIS OF ORE CONTROL CONDITIONS OF SHIPINGCHUAN MO DEPOSIT IN QINGTIAN,ZHEJIANG |
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| DONG Liang.AN ANALYSIS OF ORE CONTROL CONDITIONS OF SHIPINGCHUAN MO DEPOSIT IN QINGTIAN,ZHEJIANG[J].Yunnan Geology,2010,29(4):431-433. |
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| Authors: | DONG Liang |
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| Institution: | DONG Liang ( Geological Team 11 of Zhefiang Province, Wenzhou 325000) |
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| Abstract: | The Late Yanshanian 4th intrusive alkaline feldspar granite body provides the material source and heat energy for the Pingchuan Mo deposit. And the volcanic mechanism, fault and the 2nd rock member of Xishantou Formation provide the channel for ore transmission, the space for ore reserve in the metallogenesis. |
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| Keywords: | Altered Tuff Type Veinlet Banded Molybdenite Ore Control of Volcanic Mechanism Late Yanshanian Granite Shipingchuan Qingtian Zhejiang |
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