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- W2381733456 abstract "The Wunugetushan copper-molybdenum deposit belongs to continental subvolcanic porphyry copper-molybdenum deposit controlled by volcanic mechanism.The major fracture system consists of northeast trending and northwest trending fractures in the joining part of whom,the volcanic mechanism occurs and the ore carrying magmatic rock-sub-plagiogranite porphyry is controlled by volcanic mechanism occurring in volcanic pipe(partly intersecting volcanic pipe),being the central location of volcanic magma activities.In the meantime some ring-shaped and radiated fractures formed in the volcanic mechanism with thin or thick wall of the volcanic pipe,all providing favorable structure space for the penetration of ore bearing hot fluid and extensive replacement,resulted in the forming of facial alteration-mineralization zone.The orebodies mainly occur on the ring shaped inside and outside contact alteration zones centered at sub-plagiogranite porphyry.The multi-period supergene phase intermediate to acid subvolcanic intrusive rocks formed especially through the most serious subvolcanic activities,associated with volcanic mechanism at the volcanic-structure and magma activity center.F face-shaped alteration haloes with clear zonings of quartz-feldspar and quartz-sericite type replacement are all the main targets for the prospecting of porphyry type copper-molybdenum deposit." @default.
- W2381733456 created "2016-06-24" @default.
- W2381733456 creator A5059816886 @default.
- W2381733456 date "2007-01-01" @default.
- W2381733456 modified "2023-09-23" @default.
- W2381733456 title "Ore controlling factors of subvolcanic porphyry type coppermolybdenum deposit in Wunugetushan of Inner Mongolia,and its ore prospecting orientation" @default.
- W2381733456 hasPublicationYear "2007" @default.
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