云南地质
雲南地質
운남지질
YUNNAN GEOLOGY
2011年
3期
323-325,304
,共4页
范建辉%赵含军%李阿者
範建輝%趙含軍%李阿者
범건휘%조함군%리아자
风化淋漓残坡积%澜沧群%绿片岩相%沉积-变质改造%云南勐海盘龙山
風化淋巑殘坡積%瀾滄群%綠片巖相%沉積-變質改造%雲南勐海盤龍山
풍화림리잔파적%란창군%록편암상%침적-변질개조%운남맹해반룡산
Weathering - Leaching Sedentary - Slope Materials%Lancang Group%Sedimentary - Metamor-phic Reformation%Greenschist Facies%Panlongshan,Menghai,Yunnan
盘龙山铁矿成矿物质在热动力条件下迁移，在区域变质及构造作用下，达到绿片岩相的热动力作用下富集成矿化体，之后经漫长风化淋漓富集，原地堆积形成工业矿体，属沉积-变质改造型铁矿之风化淋漓富集残坡积矿床。
盤龍山鐵礦成礦物質在熱動力條件下遷移，在區域變質及構造作用下，達到綠片巖相的熱動力作用下富集成礦化體，之後經漫長風化淋巑富集，原地堆積形成工業礦體，屬沉積-變質改造型鐵礦之風化淋巑富集殘坡積礦床。
반룡산철광성광물질재열동력조건하천이，재구역변질급구조작용하，체도록편암상적열동력작용하부집성광화체，지후경만장풍화림리부집，원지퇴적형성공업광체，속침적-변질개조형철광지풍화림리부집잔파적광상。
Because of the process of regional metamorphism and stauctural agent, the metallogenetic body is concentrated by the thermal process of greenschist facies in Panlongshan Fe deposit. Then, the commercial ore body is formed by the weathering leaching concentration in a long term as an accumulation in situ, which belongs to the sedentary - slope materials Fe ore deposit of weathering leaching concentration of sedimentary metamorphic reformation type.
