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诸广岩体中闪长质包体的成因探讨
引用本文:徐红.诸广岩体中闪长质包体的成因探讨[J].矿物岩石,1994,14(3):16-21.
作者姓名:徐红
作者单位:南京交通专科学校
摘    要:本文对诸广关田和扶溪岩体中的闪长质包体进行了矿物岩石、岩石化学和稀土元素地球化学等方面的研究,发现这些包体是花岗质寄主岩浆自身演化的产物,包体的形成主要与寄主岩浆冷凝过程中不同组分的热扩散(Soret效应)和液相不混溶作用有关。

关 键 词:闪长质包体  热扩散  液相不混溶

DISCUSSION ON GENESIS OF DIORITIC ENCLAVES IN ZHUGUANG GRANITIC COMPLEX
Xu Hong.DISCUSSION ON GENESIS OF DIORITIC ENCLAVES IN ZHUGUANG GRANITIC COMPLEX[J].Journal of Mineralogy and Petrology,1994,14(3):16-21.
Authors:Xu Hong
Abstract:There are some dioritic enclaves distributed in Guantian and Puxi plutons in Zhuguanggtanitic complex.The characterisitics of mineralogy,petrology, petrochemistry and REE geo-chemistry of these enclaves show that they are product of self-evolution of host granitic magmas.The formation of enclaves mainly related with thermal diffusion of different components(Soreteffect)and liquid immiscibillty within host magmas during ccoling differentiation.
Keywords:dioritic enclave  thermal diffussion  magma immiscibility  
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