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白玉县炯隆寺-阿吉森多岩体成因分析
引用本文:汪友明.白玉县炯隆寺-阿吉森多岩体成因分析[J].四川地质学报,1993(3).
作者姓名:汪友明
作者单位:四川省地矿局科研所
摘    要:本文以同源岩浆演化序列的观点,探讨了炯隆寺-阿吉森多岩体的成因。研究结果表明,该岩体为印支晚期形成的同熔型花岗闪长岩-二长花岗岩,属于岛弧深成侵入的岩浆岩。

关 键 词:岛弧型深成岩  同源岩浆演化序列  同熔型花岗岩

ON PETROGENESIS OF AJISENDUO GRANITE MASS AT JIONGLONGSI,BAIYU COUNTY
Wang Youming.ON PETROGENESIS OF AJISENDUO GRANITE MASS AT JIONGLONGSI,BAIYU COUNTY[J].Acta Geologica Sichuan,1993(3).
Authors:Wang Youming
Abstract:The present paper makes an approach to petrogenesis of Ajisenduo granite mass at Jionglongsi, Baiyu County from the viewpoint of comagmatic evolutionary series. The results of the study indicate that the said mass is a syntectic granodiorite-adamellite mass formed in Late Indo-Chinese epoch, being an island arc type plutonite.
Keywords:comagmatic evolutionary series  syntectic granite  island arc type plutonite
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