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会东县菜园子磁铁矿床地质特征及成因
引用本文:徐彬.会东县菜园子磁铁矿床地质特征及成因[J].四川地质学报,2014,34(3):385-389.
作者姓名:徐彬
作者单位:四川省地矿产勘查开发局四○四队,四川西昌,615000
摘    要:菜园子磁铁矿位于扬子地台西缘康滇地轴中段东缘,江舟—米市断陷盆地带南段,川滇黔相邻成矿区之会理—会东前寒武纪铁铜铅锌银成矿远景区内。通过对该矿床地质特征、物探异常特征与见矿效果的验证、矿体地质特征、围岩蚀变的分析,认为菜园子磁铁矿床为与晋宁期中基性次火山作用有关的"火山喷溢(发)—变质热液型"(赤)磁铁矿床。

关 键 词:磁铁矿  地质特征  成因  会东

Geological Features and Genesis for the Caiyuanzi Magnetite Deposit in Huidong,Sichuan
XU Bin.Geological Features and Genesis for the Caiyuanzi Magnetite Deposit in Huidong,Sichuan[J].Acta Geologica Sichuan,2014,34(3):385-389.
Authors:XU Bin
Institution:XU Bin (No. 404 Geological Team, BGEEMRSP, Xichang, Sichuan 615000)
Abstract:The Caiyuanzi magnetite deposit in Huidong, Sichuan lies in the Huili-Huidong Precambrian Fe-Cu-Pb-Zn Metallogenetic zone on the eatem margin of the Kangdian Axis. This paper deals with geological features and geophysical characteristics as well as wall rock alteration which indicate volcanic-metamorphic hydrothermal origin related to the Jinning intermediate-basic subvolcanism.
Keywords:magnetite  geological feature  genesis  Caiyuanzi  Huidong
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