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新疆东准噶尔两类碱性花岗岩及其地质意义
引用本文:刘家远,喻亨祥,吴郭泉.新疆东准噶尔两类碱性花岗岩及其地质意义[J].矿物岩石地球化学通报,1999(2).
作者姓名:刘家远  喻亨祥  吴郭泉
作者单位:桂林工学院
基金项目:国家305项目“八五”专题
摘    要:研究证明,东准噶尔境内广泛发育的碱性花岗岩在空间上与深断裂、蛇绿岩及偏碱性的钾长花岗岩类紧密伴生,并可规律地分为卡拉麦里碱性花岗岩带(简称南带)、乌伦古碱性花岗岩带(简称中带)和布尔根碱性花岗岩带(简称北带)。南、中两带碱性花岗岩形成于海西中晚期,图...

关 键 词:碱性花岗岩  A_1、A_2型  板内裂谷环境  东准噶尔

Two Kinds of Alkaline Granites in Eastern Junggar, Xinjiang and Their Geological Significance
Liu Jiayuan,Yu Hengxiang,Wu Guoquan.Two Kinds of Alkaline Granites in Eastern Junggar, Xinjiang and Their Geological Significance[J].Bulletin of Mineralogy Petrology and Geochemistry,1999(2).
Authors:Liu Jiayuan  Yu Hengxiang  Wu Guoquan
Abstract:From the point of view of geochemistry, combined with petrological study,the paper expounds the genesis of alkaline gran ites.It is considered that three zones of alkaline granites in eastern Junggar a re similar to typical A type granites and belong to A type granites.At the sam e time,according to Eby's(1992) further dividing scheme and method cited and by means of the projection of four groups of discriminant graphic interpretations,i t is indicated that three zones of alkaline granites in eastern Junggar during d ifferent periods may be further divided into A 1 type and A 2 type subgrou nps.N zone variscan late alkaline granites are A 1 type granites formed withi n the intraplate rift environment or the rift environment.S zone and mesozone v ariscan late alkaline granites are A 2 type granites formed within the postoro genic extension structure environment.Their tectonic and metallogenic significan ce is greatly different.
Keywords:eastern Junggar  alkaline granite  A  1  A  2  type  intraplate rift environment  postorogenic  extension  structur e environment
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