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- W2373268998 abstract "The Sifangdianzi Mo deposit in Jilin Province is a recently discovered quartz-vein type molybdenum deposit.The orebodies are mainly hosted in monzogranite.Its ore-forming processes can be divided into three stages:barren quartz-vein stage,quartz-molybdenite-pyrite stage and quartzcarbonatate stage.By the LA-ICP-MS U-Pb dating of zircons,we obtained the age of 170.0±1.0 Ma for granodiorite,and the age of 179.0±1.0 Ma for monzogranite.Based on the Re-Os dating of molybdenite from quartz vein type ore,the model ages obtained are from 175.0±2.6 to 176.5±2.6Ma averaged at 176.1±1.1 Ma,and having an isochronic age of 176.6±4.2 Ma.It is indicated that the Sifangdianzi Mo deposit was formed in the early Jurassic Period.SiO2 values of the granitic rocks change from 66.17% to 76.60%,Na2O and K2O are in the range of 3.15% to 5.40% and 2.42% to 5.42% respectively,their Rittmann indexes vary from 2.17 to 2.93;Their REE patterns demonstrate rightoblique linear REE patterns,the trace elements show relative enrichment of the large ion lithophile elements,and depletion of the high field strength elements.The geochemical characteristics of the granitic rocks imply they belong to I-type granite.The geotectonic mechanisms responsible for the diagenesis and mineralization were probably related to subduction of the paleo-Pacific Plate to the Eurasian continent." @default.
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- W2373268998 date "2014-01-01" @default.
- W2373268998 modified "2023-09-24" @default.
- W2373268998 title "Diagenetic and Metallogenic Geochronology and Geochemical Characteristics of the Sifangdianzi Molybdenum Deposit in Jilin Province" @default.
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