云南地质
雲南地質
운남지질
YUNNAN GEOLOGY
2011年
4期
415-419,414
,共6页
铜铅锌多金属%矽卡岩及热液型%氧化—混合—原生带%8条矿带%青海迎庆沟-景忍东
銅鉛鋅多金屬%矽卡巖及熱液型%氧化—混閤—原生帶%8條礦帶%青海迎慶溝-景忍東
동연자다금속%석잡암급열액형%양화—혼합—원생대%8조광대%청해영경구-경인동
Cu-Pb-Zn Multimetallic%Skarn and Hydrothermal Type%Oxidate-Mixture-Original Zone%8 Ore Zones%Yingqinggou—Jingrendong%Qinghai
迎庆沟-景忍东矿区圈出8条矿带,多条主矿体,规模几近大型。成因类型复杂,从接触交代到热液型均有,亦发现斑岩型、层控型矿床类型的迹象。
迎慶溝-景忍東礦區圈齣8條礦帶,多條主礦體,規模幾近大型。成因類型複雜,從接觸交代到熱液型均有,亦髮現斑巖型、層控型礦床類型的跡象。
영경구-경인동광구권출8조광대,다조주광체,규모궤근대형。성인류형복잡,종접촉교대도열액형균유,역발현반암형、층공형광상류형적적상。
8 ore zones have been outlined in Yingqinggou—Jingrendong Orefield.The scale of many main ore bodies is near to that of large type.The genetic type is complicated,from contact metasomatic to hydrothermal type.Moreover,we have discovered the trace of ore deposit of porphyry and stratabound type.
