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《Geochimica》 2012-01
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Compositions of olivine from the mafic-ultramafic complexs in eastern Tianshan, Xinjiang and implications to petrogenesus:Examples from Huangshandong and Tulargen complexes

LIU Yan-rong1,Lü Xin-biao1,2,MEI Wei1 and HUI Wei-dong3 1.Faculty of Resource Department,China University of Geosciences,Wuhan 430074,China;2.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China;3.Xinjiang Hexin Mining Co.,Ltd,Hami 839000,China  
A dozen of mafic-ultramafic complexes related to copper-nickel sulphide mineralization were found in Eastern Tianshan,Xinjiang.This paper takes Huangshandong and Tulargen complexes for examples,and carries out mineral chemistry tests of fresh olivine from different lithologies.Electron microprobe analyses of olivine show that the Fo of olivine in hornblende-gabbro facies and ultramafic rock facies range from 67 to 73 and from 81 to 84,respectively;Ni contents range from 308 to 1762 μg/g in Huangshandong complex.Olivine crystals in the Tulargen complex have Fo numbers varying from 82 to 85,with Ni from 857 to 1818 μg/g.Modeling of olivine fractional crystallization and sulfide segregation show that the parental magma for Huangshandong complex has experienced 19% olivine fractional crystallization and extensive sulfide segregation(~0.3%).Re-equilibration of the early formed olivine crystals with trapped liquid can account for the variations of olivine compositions.The Tulargen complex has experienced 9% olivine fractional crystallization and extensive sulfide segregation(~0.5%).
【Fund】: “十二五”国家科技支撑计划项目(2011BAB06B04-05)
【CateGory Index】: P588.125
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