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广西大容山-十万大山岩带中花岗岩类特征及成因
引用本文:汪绍年.广西大容山-十万大山岩带中花岗岩类特征及成因[J].岩石学报,1991(2).
作者姓名:汪绍年
作者单位:广西地质学校 南宁
摘    要:大容山-十万大山花岗岩带由花岗岩、花岗斑岩和少量混合花岗岩、酸性火山岩组成,它们共同构成一个原地半原地→中深成侵入→浅成侵入→喷出相的完整花岗岩类成因系列。这些岩石在矿物组成、化学成分、微量和稀土元素以及同位素组成上十分相似,都来源于上部地壳,属陆壳转生型花岗岩,其源岩是由角闪岩相到麻粒岩相的变质沉积岩。

关 键 词:花岗岩类  岩石成因  岩石系列  大容山-十万大山岩带  广西

CHARACTERISTICS AND GENESIS OF GRANITOIDS IN THE DARONGSHAN AND SHIWANDASHAN AREA OF GUANXI PROVINCE, CHINA
Wang Shaonian.CHARACTERISTICS AND GENESIS OF GRANITOIDS IN THE DARONGSHAN AND SHIWANDASHAN AREA OF GUANXI PROVINCE, CHINA[J].Acta Petrologica Sinica,1991(2).
Authors:Wang Shaonian
Abstract:Granitoids in the regions of Darongshan and Shiwandashan are composed mostly of granites, granite-pophyry and some migmatitie granites,and acidic volcanic rocks as well. The similarity of these rocks in mineralogical and chemical compositions and in Sr-Nd-O isotopes suggests that they were likely derived from the same sources and assemble a rock series of granitoids ineluding plutonic rocks, hypabyssal rocks and eruptive ones.The source rocks of them are metasedimentary rocks of amphibolite-granulite faces.
Keywords:Granitoids  rock series  Petrogenesis  
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