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内蒙古满洲里地区中生代中基性火山岩成因及构造地质背景
引用本文:李长华,卫三元,陈贵海,翁义军,姜山,杨志亮.内蒙古满洲里地区中生代中基性火山岩成因及构造地质背景[J].国外铀金地质,2010(1):19-24.
作者姓名:李长华  卫三元  陈贵海  翁义军  姜山  杨志亮
作者单位:[1]核工业243大队,内蒙古赤峰024006 [2]核工业北京地质研究院,北京100029
摘    要:内蒙古满洲里地区位于大兴安岭中生代火山岩带的中北段,晚侏罗世—早白垩世火山岩浆活动强烈,由于NE向切壳断裂长期活动,导致中基性火山岩沿断裂呈线状分布。就上侏罗统塔木兰沟组、上库力组中段及下白垩统伊列克得组中基性火山岩浆岩的组合、旋回和岩石地球化学等方面的特征,论证了该地区中生代中基性火山岩浆岩形成的构造地质背景和成因。因此,认为晚侏罗世中基性火山岩形成于板内拉张的构造环境,岩浆来源于上地幔,且有地壳物质混熔。

关 键 词:满洲里地区  中基性火山岩  构造环境  岩浆来源

Genesis and tectonic geological setting of Mesozoic intermediate-basic volcanics in Manzhouli region,Inner Mongolia
Authors:LI Chang-hua  WEI San-yuan  CHEN Gui-hai  WENG Yi-jun  JIANG Shan  YANG Zhi-liang
Institution:1. Geologic Party No.243,CNNC,Chifeng,Inner Mongolia 024006,China; 2. Beijing Research Institute of Uranium Geology,Beijing 100029,China)
Abstract:Manzhouli region in Inner Mongolia is located at the mid-northern segment of Mesozoic volcanic belt in Da Xing'anling area. Due to the long-term activities of a NE-trending crustal fault,Late Jurassic-Early Cretaceous volcanic magma activity of intermediate-basic volcanics is strong and distributes along the fault as linear. Through analyzing the feature of the rock assemblage,cycles and petrogeochemistry of volcanic magmatism in Upper Jurassic Tamulangou Formation,middle segment of Upper Kuli Formation and Lower Cretaceous Yiliekede Formation,the tectonic geological setting and magama genesis are elaborated,Late Jurassic volcanics is considered to form in the tectonic setting of intraplate tension and the magma comes from the upper mantle with some melted crustal materials.
Keywords:Manzhouli region  intermediate-basic volcanics  tectonic environment  magma sources
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