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- W2393065478 abstract "Carboniferous volcanic rocks from Qietemusi copper deposit in western Tianshan Mountains are composed of high potassium calc-alkalic andesite.These rocks characterized by high SiO2,Al2O3,Sr and low MgO,Y,Yb contents are similar to O-type adakite.And its geochemical characteristics show that they are enriched in LREE relative to HREE,as well as fractionated rare earth elements(REE),and also enriched large-ion-lithophile elements(LILE) such as Rb,Ba,Th,K,strongly depleted high-field-strength elements(HFSE) such as Nb,Ta and Ti.This indicates that they have an obviously blood relationship with volcanic-arc rocks and may be related to the subduction of the South Tianshan Ocean towards north beneath the Yili-Central Tianshan plate.Compared to Tuwu-Yandong porphyry copper deposit in eastern Tianshan Mountains,the Qietemusi volcanic rocks have the similar geochemical character and tectonic setting.Furthermore,crypto-explosion breccias,alteration patterns of porphyry copper deposits and low erosion level indicate that the exploration potentiality of porphyry copper deposit is remarkable." @default.
- W2393065478 created "2016-06-24" @default.
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- W2393065478 date "2011-01-01" @default.
- W2393065478 modified "2023-09-23" @default.
- W2393065478 title "GEOCHEMICAL CHARACTERISTICS AND METALLOGENIC BACKGROUND OF CARBONIFEROUS VOLCANIC ROCKS FROM QIETEMUSI COPPER DEPOSIT,WESTERN TIANSHAN,XINJIANG" @default.
- W2393065478 hasPublicationYear "2011" @default.
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