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- W2361791851 abstract "From the characterstics on Lothochemistry and geochemistry,it is found out that the Geological features of the Xiaojyayingzi intrusion and Molybdenum polymetallic deposit,gabbro-diabase-porphyry fine diorite of Xiaojiayingzi ore district belong to Yenshanion period(177～113 Ma).It is an integrated intrusion which is deep-seated,syngenetic,rich in trace elements and Volatile compounds and obviously low compared with other intrusion SiO 2 content of intrusion of the typical porphyry type molybdenum deposit in China,Molybdenum polymetallic orebodies and alteration occur within the gabbro-diabase-porphyry fine diorite porphyry body.There exists in a half circle around the intrusion molybdenum polymetallic mineralization closely related with intrusion alteration.The temperatures for the mineralization are 250～400℃.δ 34S 1.1‰～4.4‰.The sulfur isotopic composition of Xialjiayingzi intrusion and orebodies are uniform.The ore-forming substances are derived from the porphyry fine diorite which intrudes later. With the ore-fluid evoluted,dissipated,transferred thus forms the porphyry molybdenum orebodies.skarn molybdenum copper Iron orebodies.fissure metasomatic-filling sliver lead zinc orebodies.All in all Xiaojiayingzi molybdenum polymetallic deposit is an integrated porphyry type deposit." @default.
- W2361791851 created "2016-06-24" @default.
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- W2361791851 date "2002-01-01" @default.
- W2361791851 modified "2023-09-25" @default.
- W2361791851 title "On geological features and genesis of the Xiaojiayingzi molybdenum polymetallic deposit in Liaoning" @default.
- W2361791851 hasPublicationYear "2002" @default.
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