| 福建浦城金竹坑铅锌矿床地质特征及成因初探 |
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| 引用本文： | 刘乃忠,刘诗光.福建浦城金竹坑铅锌矿床地质特征及成因初探[J].福建地质,2004,23(2):59-66. |
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| 作者姓名： | 刘乃忠 刘诗光 |
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| 作者单位： | 福建省地质测绘院,福州,350011;福建省地质测绘院,福州,350011 |
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| 摘 要： | 浦城金竹坑铅锌矿床产于早元古代麻源群大金山组、大金山组与侏罗系梨山组接触带以及加里东期片麻状花岗闪长岩中。矿体呈脉状、似层状，受断裂构造控制，成矿在时问、空问上与中生代中酸性岩浆活动密切相关，属于岩浆热液交代一充填式矿床。
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| 关 键 词： | 铅锌矿 矿床地质特征 脉状似层状 浦城金竹坑 |
| 修稿时间： | 2003年11月15 |
Geologic Characteristics and Genesis of the Jinzhukeng Lead-zinc Deposit in Pucheng County, Fujian Province |
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| Liu Naizhong,Liu Shiguang.Geologic Characteristics and Genesis of the Jinzhukeng Lead-zinc Deposit in Pucheng County, Fujian Province[J].Geology of Fujian,2004,23(2):59-66. |
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| Authors: | Liu Naizhong Liu Shiguang |
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| Abstract: | The Jinzhukeng Lead zinc Deposit in Pucheng County is distributed in the Proterozoic strata of Mayuan Group Dajianshan Formation and the contact zones of Dajianshan Formation and Jurassic Lishan Formation and in Caledonian gneissoid granodiorite The orebodies of the Jinzhukeng Lead zinc Deposit, as a veiny and bedded shape, are controlled by faulted structures and have a close relation with Mesozoic intermediate acid magmation in time and space, which belongs to a deposit of the magmatic hydrothermal replacement and filling type |
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| Keywords: | lead-zinc deposit geologic characteristics veiny orebody stratiform Pucheng County |
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