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四川省冕宁县大顶山磁铁矿床成因探讨
引用本文:范元建,侯立平,杨璐,李松键.四川省冕宁县大顶山磁铁矿床成因探讨[J].地质找矿论丛,2014,29(4):546-551.
作者姓名:范元建  侯立平  杨璐  李松键
作者单位:四川省冶金地质勘查院,成都,610051
基金项目:危机矿山接替资源找矿、老矿山专项“四川省冕宁县泸沽铁矿接替资源勘查”项目
摘    要:大顶山磁铁矿床位于泸沽花岗岩体外接触带,铁矿体赋存于中元古界登相营群夕卡岩化大理岩中,呈似层状、透镜状产出,矿体与夕卡岩化大理岩关系密切;大顶山磁铁矿床是泸沽花岗岩体侵位过程中沿层交代的产物,其矿床成因属接触交代型矿床.

关 键 词:大顶山磁铁矿  地质特征  矿床成因  接触交代  四川省
收稿时间:2013/4/28 0:00:00
修稿时间:2014/7/3 0:00:00

Discuss ion on the genesis of Dadingshan magnetite ore deposit in Mianning county, Sichuan province
FAN Yuanjian,HOU Liping,YANG Lu and LI Songjian.Discuss ion on the genesis of Dadingshan magnetite ore deposit in Mianning county, Sichuan province[J].Contributions to Geology and Mineral Resources Research,2014,29(4):546-551.
Authors:FAN Yuanjian  HOU Liping  YANG Lu and LI Songjian
Institution:FAN Yuanjian; HOU Liping; YANG Lu;LI Songjian (Metallurgical Geological Institute Sichuan Province, Chengdu 610051, China)
Abstract:Dadingshan magnetite ore deposit is located in outer contact zone of Lugu granite body. The iron ore bodies occur in layeroid body or lens in the skarnized marble of Middle Proterozoic Dengxiangying group and are closely related to the skarnized marble. Dadingshan magnetite deposit is the product of metasomatism along bed plane during emplacement of the Lugu granite
Keywords:Dadingshan magnetite ore deposit  geologic feature  genesis of the deposit  contact metasomatism  Sichuan province
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