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汪清县六道崴子地区碱长花岗岩地质特征及构造背景分析
引用本文:孔祥晶.汪清县六道崴子地区碱长花岗岩地质特征及构造背景分析[J].吉林地质,2014(2):26-30.
作者姓名:孔祥晶
作者单位:吉林省勘察地球物理研究院,吉林长春130012
摘    要:分布在汪清县六道崴子地区的碱长花岗岩,研究后认为是A型花岗岩。其特征是具晶洞构造,钾长石是中正微长石,斜长石为钠长石(An=1),SiO2、K2O、Na2O质量分数较高,CaO、MgO质量分数较低。∑REE质量分数为139.3,δEu为0.14,亏损十分明显,是非造山期拉张构造环境形成的碱性花岗岩。

关 键 词:汪清县六道崴子地区  碱长花岗岩  A型花岗岩  构造环境

Geological features and tectonic background of Alkali feldspar granite in Liudaowaizi area of Wangqing County
KONG Xiang-jing.Geological features and tectonic background of Alkali feldspar granite in Liudaowaizi area of Wangqing County[J].Jilin Geology,2014(2):26-30.
Authors:KONG Xiang-jing
Institution:KONG Xiang-jing (Institute of Geophysical Exploration of Jilin Province, Changchun 130012, Jilin, China)
Abstract:After researching, alkali feldspar granite that located in Liudaowaizi area of Wangqing County, is A type granite, which with miarolitic structure, potassium feldspar is microcline, plagioclase is albite (An=1), the mass fraction of SiO2, K2O, Na2O are high, which of CaO, MgO are low. The mass fraction of∑REE is 139.3,δEu is 0.14, its loss is obvious. That is alkali granite formed in extensional tectonic environment of non orogenic period.
Keywords:Liudaowaizi area of Wangqing County  alkali feldspar granite  A type granite  tectonic environment
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