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《Global Geology》 2017-02
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Zircon U-Pb geochronology,petrogeochemistry and tectonic significance of volcanic rocks from Tamulangou Formation in western Huzhong,northern Great Xing'an Range

YANG Nai-feng;YANG Li-ting;Heilongjiang Mining Group Co.,Ltd;Heilongjiang Provincial Geology and Mineral Resources Test and Application Institute;  
Huzhong volcanic rock belt lies in the northern part of Greater Khingan Range.Tamulangou Formation,which is one of the earlier phases of the eruption,is mainly composed of intermediate-basic volcanic rock.Zircon U-Pb dating shows that the Huzhong volcanic rock formed in the Late Jurassic(154 ± 1 Ma).SiO_2 content of Huzhong volcanic rock is 49.80% ~ 55.96%,Al_2O_3 is 16.70% ~ 18.93%,Na_2O + K_2O is 6.35% ~9.11%,belonging to intermediate-basic high alumina alkaline rocks.The volcanic rocks are enriched in large ion lithophile elements Ba,and depleted in Nb,Ta,with Nb/Ta = 12.44 ~ 15.58.The changes of Huzhong volcanic rock element contents and their ratios indicate that the basaltic magma of Tamulangou Formation is influenced by crust-derived material during fractional crystallization process.The formation was formed in the plate margin arc orogen environment related to the subduction of Paleo Asian Ocean plate and(or) Mongolia--Okhotsk Ocean plate.
【Fund】: 黑龙江省资源补偿项目(HLJKD2007-01)
【CateGory Index】: P597;;P595
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