| 李祥能.湖南后江桥铅锌矿地质特征及矿床成因[J].地质找矿论丛,2002,(1):41-46 |
| 湖南后江桥铅锌矿地质特征及矿床成因 |
| DEPOSIT GENESIS AND GEOLOGICAL CHARACTERISTICS OF HOUJIANGQIAO Pb-Zn DEPOSIT IN HUNAN |
| 投稿时间：2001-08-22 修订日期：2001-12-13 |
| DOI：10.6053/j.issn.1001-1412.2002.1. 005 |
| 中文关键词: 后江桥 铅锌矿 地质特征 矿床成因 湖南省 |
| 英文关键词:Hou Jiangqiao Pb-Zn deposit Geological characteristics Deposit genesis Hunan |
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| 中文摘要: |
| 后江桥铅锌矿具有多源、多阶段成矿特点,成矿主要与泥盆纪地层及热液作用有关。对其矿床地质特征、同位素地质学、矿床成因等方面研究,认为成矿物质来源具双重性,既有来源于地层,又有来自壳幔源岩浆。成因类型属于沉积改造型铅锌矿床。 |
| 英文摘要: |
| The Houjiangqiao Pb-Zn deposit features multi-source, multi-stage in mineralization, which is mainly related to Devonian strata and hydrothermal activity. Studies on geology, isotopes and metallogenesis indicate that the ore-forming material derived from strata and magma derived from crust-mantle. The deposit belongs to Pb-Zn deposit related to sedimentary-remobilization. |
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