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- W2393178150 abstract "More than 14 Mo ore prospects in eastern Qinling,central China,occur in a mineralization zone with a length of 200 km and a width of 20 km.The Mo deposits are hosted mainly in small intermediate-acid intrusions of Cretaceous age.These intrusions are composed dominantly of granoporphyry and quartz monzonite.The major types of deposits include:(1) porphyry-type Mo deposits,(2) porphyry-skarn-type Mo deposits,(3) skarn-type Mo deposits,(4) vent breccia-type Mo deposits,and(5) hydrothermal vein-type Mo deposits.Regional geology and deep-seated structures show that there is a mantle depression structure(the Luanchuan mantle syncline) beneath the Mo mineralization zone along an E-W striking axis and it dips westwards.The northern flank of the mantle depression links the Luoyang mantle uplift,which was distorted northwards to develop a set of NE-striking extension-shear faults,overlaping the EW-extending deep-seated faults parallel to the ancient continental margins.The two groups of faults then formed a check-shaped deep-seated fault assemblage,of which the intersection areas provided the ascending channels and precipitation spaces for ore fluids derived from crust-mantle interaction and controlled the emplacement of a series of intermediate-acid granite magmas and thereafter mineralization." @default.
- W2393178150 created "2016-06-24" @default.
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- W2393178150 date "2007-01-01" @default.
- W2393178150 modified "2023-09-23" @default.
- W2393178150 title "MOLYBDENUM DEPOSITS IN EASTERN QINLING,CENTRAL CHINA:DEEP STRUCTURAL CONSTRAINTS ON THEIR FORMATION" @default.
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