Resources & Industries ›› 2008, Vol. 10 ›› Issue (6): 119-124.
• STUDY ON PROBLEMS • Previous Articles
PENG Xiao-ming
(Fujian No.4 Geological Brigade, Ningde 352100, China)
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彭晓明
(福建省第四地质大队,福建 宁德 352100)
作者简介:
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
lead-zinc polymetallic deposit; geology; genesis; Baliqiao in Jiangle
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
CLC Number:
P618.4
PENG Xiao-ming. GEOLOGY AND GENESIS OF BALIQIAO LEADZINC PLOYMETALLIC DEPOSIT IN JIANGLE[J]. Resources & Industries, 2008, 10(6): 119-124.
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.
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