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河南栾川中鱼库矽卡岩矿物学特征及地质意义

胡昕凯 张寿庭 曹华文 裴秋明 夏炳卫 赵玉 王亮

成都理工大学学报(自然科学版)2017,Vol.44Issue(3):318-333,16.
成都理工大学学报(自然科学版)2017,Vol.44Issue(3):318-333,16.DOI:10.3969/j.issn.1671-9727.2017.03.05

河南栾川中鱼库矽卡岩矿物学特征及地质意义

Characteristics and geological significance of skarn minerals from the Zhongyuku sulfide-zinc polymetallic deposit in Luanchuan, Henan, China

胡昕凯 1张寿庭 1曹华文 2裴秋明 1夏炳卫 1赵玉 1王亮1

作者信息

  • 1. 中国地质大学地球科学与资源学院,北京100083
  • 2. 中国地质调查局成都地质调查中心,成都610081
  • 折叠

摘要

Abstract

Systematic field work,microscopic identification and electron microprobe technology are carried out to study the mineralogical characteristics of skarn and to discuss the petrogenic and metallogenic mechanism in the Zhongyuku sulfide-zinc polymetallic deposit.It reveals that the ore deposit has experienced four ore-forming stages,such as skarn stage,retrograde alteration stage,quartz sulfide stage and carbonate stage,respectively.The skarns in the Zhongyuku deposit belong to typical calcic skarns resulted from the replacement of granitoid magma.Garnets in the ore deposit are mainly composed of andradite-grossularite and the pyroxenes mainly belonging to diopside-andradite series.Amphiboles in the ore show characteristics of calciferous amphibole,and the chlorites are mainly brunsvigite.Components of garnet and pyroxene suggest that the ore-forming fluid have an evolutionary trend from acidic to basic and from reduction to oxidation condition at the skarn stage.From the retrograde alteration stage to the quartz sulfide stage,the oxygen fugacity drops with the evolutionary of ore-forming fluid.The metal sulfides are precipitated at the quartz sulfide stage.

关键词

矽卡岩/矿物学/硫锌多金属矿床/中鱼库

Key words

skarn/mineralogy/sulfide-zinc polymetallic deposit/Zhongyuku

分类

天文与地球科学

引用本文复制引用

胡昕凯,张寿庭,曹华文,裴秋明,夏炳卫,赵玉,王亮..河南栾川中鱼库矽卡岩矿物学特征及地质意义[J].成都理工大学学报(自然科学版),2017,44(3):318-333,16.

基金项目

中国地质调查局地质调查项目(1212011220925) (1212011220925)

国家“十二五”科技支撑计划项目(2011BAB04B06). (2011BAB04B06)

成都理工大学学报(自然科学版)

OA北大核心CSCDCSTPCD

1671-9727

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