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南秦岭东江口岩体闪长质包体地球化学特征及成因探讨
引用本文:朱茂旭,骆庭川.南秦岭东江口岩体闪长质包体地球化学特征及成因探讨[J].矿物岩石,1997,17(2):28-34.
作者姓名:朱茂旭  骆庭川
作者单位:中国科学院地球化学研究所,中国地质大学地球化学研究所
摘    要:本文对南秦岭东江口岩体中的闪长质包体的主量元素,微量元素地球化学特征及包体形成的温度和压力条件进行分析,揭示出闪长质包体与寄主岩体是同源的混溶包体。根据新的成因解释,认为不混溶包体的形成机理是由均一岩浆在演化过程中长英质岩浆和铁镁质岩浆有序化的结果。在有序化过程中,其具体过程可能是复杂的

关 键 词:闪长质包体  同源  不混溶  有序化

DISCUSSING ON THE GEOCHEMICAL FEATURES AND GENESIS FOR DIORITIC ENCLAVES IN DONGJIANGKOU PLUTON, SOUTHERN QINLING
Zhu Maoxu,Luo Tingchuan,Zhang Hongfei.DISCUSSING ON THE GEOCHEMICAL FEATURES AND GENESIS FOR DIORITIC ENCLAVES IN DONGJIANGKOU PLUTON, SOUTHERN QINLING[J].Journal of Mineralogy and Petrology,1997,17(2):28-34.
Authors:Zhu Maoxu  Luo Tingchuan  Zhang Hongfei
Institution:Zhu Maoxu * Luo Tingchuan ** Zhang Hongfei ** *
Abstract:In this paper based on the research for the chemical compostions,geochemical features of trace element and forming temperature and pressure of dioritic enclaves in Dongjiangkou pluton, it is reveals that the enclaves are homologous with host pluton,and are liquid immiscible ones.Besides, it is indicated the forming mechanism of enclaves as a resulted of the ordering of felsic and femic end members which may be complex during the evolution of homogeneous magma.
Keywords:dioritic enclaves\ homology\ immiscibility\ ordering
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