| 福建省丁家山铅锌矿床地质特征及成因 |
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| 引用本文： | 陈小华.福建省丁家山铅锌矿床地质特征及成因[J].福建地质,2000,19(2):57-65. |
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| 作者姓名： | 陈小华 |
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| 作者单位： | 华东有金地质勘查局,南京 |
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| 摘 要： | 研究丁家山铅锌矿的地质特征、矿物组成、稳定同位素、微量元素等表明，它是一个主要产于中元古代马面山群龙北溪组上段绿片岩系中，可划分为火山喷发（主成矿期）、变质、改造叠加、表生４个成矿期的ＶＨＳ型铅锌矿床，并具有４条明显的找矿标志。
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| 关 键 词： | 龙北溪组 成矿期 VHS型锌矿床 福建 |
Geological Features and Genesis of Dingjiashan Pb-Zn Deposit in Fujian Province |
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| Chen Xiaohua.Geological Features and Genesis of Dingjiashan Pb-Zn Deposit in Fujian Province[J].Geology of Fujian,2000,19(2):57-65. |
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| Authors: | Chen Xiaohua |
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| Abstract: | Based on the geological features,mineral composition,stable isotopes and microelements of the Dingjiashan Pb Zn Deposit,it shows that the Dingjiashan Pb Zn Deposit is a VHS type Pb Zn one,which exists in the greenschist series of Longbeixi Formation(upper member)of Middle Proterozoic Mamianshan Group.The Deposit can be divided into four mineralization epochs of volcanic explosion,metamorphism,superposition and supergene.There are four obvious indicators for the Deposit. |
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| Keywords: | Longbeixi Formation mineralization stage VHS type Pb Zn deposit Fujian Province |
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