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牟定大湾山磁铁矿成矿规律
引用本文:李石英.牟定大湾山磁铁矿成矿规律[J].云南地质,2014(1):85-90.
作者姓名:李石英
作者单位:云南省有色地质局楚雄勘查院,楚雄675000
摘    要:牟定安益地区元古界变质岩地层出露广泛,“大湾山式”贫磁铁矿产于元古界龙川群路古模组第三段浅变质含磁铁绿片岩中,地面高精度磁测异常与含矿地层吻合较好,矿床类型属中基性火山—沉积变质型贫磁铁矿.经多年工作,该类矿床规模已达中—大型,区内具有较好的找矿前景.

关 键 词:火山—沉积变质型贫磁铁矿  云南牟定大湾山

METALLOGENESIS RULE OF DAWANSHAN MAGNETITE DEPOSIT,MOUDING
LI Shi-ying.METALLOGENESIS RULE OF DAWANSHAN MAGNETITE DEPOSIT,MOUDING[J].Yunnan Geology,2014(1):85-90.
Authors:LI Shi-ying
Institution:LI Shi-ying ( chuxiong Exploration Institute, Yunnan Bureau of Nonferrous Geology, Chuxiong 675000)
Abstract:Proterozoic metamorphic rocks are widely outcropped in Anyi area of Mouding. "Dawan-type" poor magnetite deposit is in the epimetamorphic magnetite-beating greenschist of Proterozoic Longehuan Group Gu- mo Formation Member Ⅲ, the surface high precision magnetic anomaly is very consistent with the ore-beating bed, the ore deposit belongs to the intermediate-basic volcanic--sedimentary metamorphic type poor magnetite depos- it. The ore deposit has become medium-large scale by the exploration in many years, with good prospecting potenti- ality.
Keywords:Volcanic--Sedimentary Metamorphic Type Poor Magnetite Deposit  Dawanshan  Mouding
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