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石英脉型辉钼矿矿床多建造地球化学异常特征 |
朱柏松, 王成良, 张方君 |
浙江省第七地质大队, 浙江 丽水 323000 |
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MULTI-FORMATION GEOCHEMICAL ANOMALIES OF QUARTZ VEIN TYPE MOLYBDENITE DEPOSITS |
ZHU Bai-song, WANG Cheng-liang, ZHANG Fang-jun |
No.7 Geological Party of Zhejiang Province, Lishui 32300, China |
引用本文: |
朱柏松, 王成良, 张方君. 石英脉型辉钼矿矿床多建造地球化学异常特征[J]. 物探与化探, 2004, 28(2): 114-115,118.
ZHU Bai-song, WANG Cheng-liang, ZHANG Fang-jun. MULTI-FORMATION GEOCHEMICAL ANOMALIES OF QUARTZ VEIN TYPE MOLYBDENITE DEPOSITS. Geophysical and Geochemical Exploration, 2004, 28(2): 114-115,118.
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https://www.wutanyuhuatan.com/CN/
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https://www.wutanyuhuatan.com/CN/Y2004/V28/I2/114
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[1] 阮天健,朱有光.地球化学找矿[M].北京:地质出版社,1985.
[2] 吴光明,杨卫东.岭脚钼矿床地质特征及找矿远景分析[J].浙江地质,1999,(2).
[3] 周俊法.八宝山火山岩型金银原生晕地球化学异常特征[J].地质与勘探,1989,(1). |
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