| 福建浦城上厂钼矿床地质特征及成因初探 |
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| 引用本文： | 刘乃忠.福建浦城上厂钼矿床地质特征及成因初探[J].福建地质,2005,24(3):141-146. |
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| 作者姓名： | 刘乃忠 |
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| 作者单位： | 福建省地质调查研究院,福州,350011 |
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| 摘 要： | 浦城上厂钼矿床产于北北西和北东向2组断裂交汇处,矿体总体呈北北东向长椭圆状小岩株,长轴方向呈北东18,°长约800 m,宽约230 m。成矿与燕山晚期中偏酸性斑岩体密切相关,为斑岩型钼矿床。
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| 关 键 词： | 矿床地质特征 钼矿 斑岩型 浦城上厂 |
| 收稿时间： | 2005-04-10 |
| 修稿时间： | 2005年4月10日 |
On the Geologic Characteristics and Genesis of the Shuangchang Molybdenum Deposit in Pucheng County, Fujian Province |
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| Liu Naizhong.On the Geologic Characteristics and Genesis of the Shuangchang Molybdenum Deposit in Pucheng County, Fujian Province[J].Geology of Fujian,2005,24(3):141-146. |
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| Authors: | Liu Naizhong |
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| Abstract: | The Shangchang molybdenum deposit in Pucheng County consists in the interjunction of north-northwestern and Northeastern faults and its orebody occurs as a small oblong stock-like with the north-northeast trend, which is 800mm long and 230m wide. The ore-forming process has a close relation with the Late Yanshania intermediate-metaacid porphyritic rock and it belongs to the porphyry-type molybdenum deposit. |
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| Keywords: | geologic characteristics of a deposit molybdenum minerals porphyritic type Pucheng County |
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