将乐八里桥铅锌多金属矿地质特征及成因初探

资源与产业 ›› 2008, Vol. 10 ›› Issue (6): 119-124.

• 问题研究 • 上一篇

将乐八里桥铅锌多金属矿地质特征及成因初探

彭晓明

(福建省第四地质大队，福建宁德 352100）

收稿日期:2008-07-25 修回日期:2008-10-25 出版日期:2009-01-05 发布日期:2008-12-20
作者简介:彭晓明 (1974— )，男，工程师，主要从事地质矿产勘查。E-mail：fox21931@126.com

GEOLOGY AND GENESIS OF BALIQIAO LEADZINC PLOYMETALLIC DEPOSIT IN JIANGLE

PENG Xiao-ming

(Fujian No.4 Geological Brigade, Ningde 352100, China)

Received:2008-07-25 Revised:2008-10-25 Online:2009-01-05 Published:2008-12-20

摘要/Abstract

摘要：

八里桥铅锌多金属矿位于将乐—宁化钨、锡多金属成矿带上，产于三叠系下统溪口组地层中，矿体呈似层状—透镜状，赋存于北东向含矿断裂与矽卡岩或大理岩的相交复合部位，属于矽卡岩—热液充填型脉状铅锌（铁）多金属矿床。

关键词: 铅锌多金属矿;地质特征;矿床成因;将乐八里桥

Abstract:

Baliqiao lead-zinc polymetallic deposit which is located in Jiangle-Ninghua W-Sn polymetallic mineralization zone occurs in the lower Triassic Xikou formation. The ore bodies as lens or stratified are hosted in the conjunction between NE-striking mineralization-related faults and skarn or marble, so the deposit in genesis belongs to skarn-hydrothermal filling vein-like lead-zinc (iron) polymetallic deposit.

Key words:

lead-zinc polymetallic deposit; geology; genesis; Baliqiao in Jiangle

中图分类号:

P618.4

彭晓明. 将乐八里桥铅锌多金属矿地质特征及成因初探[J]. 资源与产业, 2008, 10(6): 119-124.

PENG Xiao-ming. GEOLOGY AND GENESIS OF BALIQIAO LEADZINC PLOYMETALLIC DEPOSIT IN JIANGLE[J]. Resources & Industries, 2008, 10(6): 119-124.

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将乐八里桥铅锌多金属矿地质特征及成因初探

GEOLOGY AND GENESIS OF BALIQIAO LEADZINC PLOYMETALLIC DEPOSIT IN JIANGLE

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