| 阳储岭钨钼矿床几种矿物的特征及与矿床成因关系 |
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| 引用本文： | 曾纪伦,曾卫胜.阳储岭钨钼矿床几种矿物的特征及与矿床成因关系[J].矿物学报,1986(3). |
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| 作者姓名： | 曾纪伦 曾卫胜 |
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| 作者单位： | 江西省地质矿产局实验测试中心 南昌
(曾纪伦)，江西省地质矿产局实验测试中心 南昌(曾卫胜) |
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| 摘 要： | 阳储岭斑岩钨钼矿床的成因特点是物理化学条件多变,同化作用和混杂作用较强。其工业矿物有白钨矿和辉钼矿,其共生矿物以金属硫化物为主。钨钼矿物及其共生矿物与矿床的成因密切相关。
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| 关 键 词： | 白钨矿 辉钼矿 矿床成因论 中酸性杂岩 江西 |
CHARACTERISTICS AND GENESIS OF SOME ORE AND ACCESSORY MINERALS IN YANGCHULING W-MO DEPOSIT |
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| Zeng Jilun,Zeng Weisheng Testing Centre,Bureau of Geology and Mineral Resources,Jiangsi.CHARACTERISTICS AND GENESIS OF SOME ORE AND ACCESSORY MINERALS IN YANGCHULING W-MO DEPOSIT[J].Acta Mineralogica Sinica,1986(3). |
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| Authors: | Zeng Jilun Zeng Weisheng Testing Centre Bureau of Geology and Mineral Resources Jiangsi |
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| Abstract: | Yangchuling porphyry W-Mo deposit is characterized by the great varietyof phicochemical conditions that prevailed during its formation'and well-deve-loped assimilation and contamination.Industrial minerals are scheelite and mo-1ybdenite with sulfides as major associated minerals. Genetically, the forma-tion of these minerals is closely related with the history of the deposit as awhole. |
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| Keywords: | scheelite molybdenite minerogenesis medium-acid complex Jiangxi |
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