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内蒙古扎鲁特盆地坤都地区满克头鄂博组流纹岩锆石U-Pb年龄及岩石成因
引用本文:张超,张渝金,权京玉,郭威,郭建刚,王青召,李伟,汪岩,宋维民,那福超,谭红艳.内蒙古扎鲁特盆地坤都地区满克头鄂博组流纹岩锆石U-Pb年龄及岩石成因[J].地质通报,2018,37(9):1633-1643.
作者姓名:张超  张渝金  权京玉  郭威  郭建刚  王青召  李伟  汪岩  宋维民  那福超  谭红艳
作者单位:中国地质调查局沈阳地质调查中心;吉林大学地球科学学院;东北煤田地质局沈阳测试研究中心
基金项目:中国地质调查局项目《内蒙古1∶5万陶海营子等四幅区域地质矿产调查》(编号:DD20160048-04)、《太平洋构造域北段构造格局、演化历史研究及1∶250万构造图编制》(编号:DD20160343-08)和《古亚洲洋构造域东段构造格局、演化历史研究及1∶250万构造图编制》(编号:DD20160343-09)
摘    要:为研究内蒙古扎鲁特盆地坤都地区晚侏罗世火山岩的构造属性,对研究区内流纹岩开展了锆石U-Pb定年和原位Lu-Hf同位素研究。锆石U-Pb定年结果显示,流纹岩形成于151.2±1.2Ma,属于晚侏罗世。岩石地球化学研究表明,火山岩具高硅富碱、贫镁钙的特征,稀土元素总量为110.38×10~(-6)~138.88×10~(-6),轻、重稀土元素分馏中等,弱负Eu异常(δEu=0.72~0.98),微量元素特征为富集Cs、Rb、Ba和轻稀土元素,强烈亏损Sr、P、Ti,相对亏损Nb、Ta,ε_(Hf)(t)值为-10.1~4.9,对应的地壳模式年龄(T~C_(DM))为1192~3639Ma,反映其岩浆来源于元古宙、太古宙地壳物质的部分熔融,之后经历矿物分离结晶作用。通过对比大兴安岭地区同时代岩浆-构造活动,研究区满克头鄂博组流纹岩形成于后造山伸展背景,与蒙古-鄂霍茨克造山后伸展作用有关。

关 键 词:扎鲁特盆地  晚侏罗世  流纹岩  满克头鄂博组  锆石U-Pb定年  Hf同位素
收稿时间:2018/3/20 0:00:00
修稿时间:2018/6/28 0:00:00

Zircon U-Pb geochronology and petrogenesis of rhyolites in Manketouebo Formation from the Kundu area in Jarud Basin, Inner Mongo-lia
ZHANG Chao,ZHANG Yujin,QUAN Jingyu,GUO Wei,GUO Jiangang,WANG Qingzhao,LI Wei,WANG Yan,SONG Weimin,NA Fuchao and TAN Hongyan.Zircon U-Pb geochronology and petrogenesis of rhyolites in Manketouebo Formation from the Kundu area in Jarud Basin, Inner Mongo-lia[J].Geologcal Bulletin OF China,2018,37(9):1633-1643.
Authors:ZHANG Chao  ZHANG Yujin  QUAN Jingyu  GUO Wei  GUO Jiangang  WANG Qingzhao  LI Wei  WANG Yan  SONG Weimin  NA Fuchao and TAN Hongyan
Institution:Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, Liaoning, China;College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China,Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, Liaoning, China;College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China,Shenyang Tests Research Center, Northeast China Coal Field Geology Bureau, Shenyang 110016, Liaoning, China,Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, Liaoning, China,Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, Liaoning, China,Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, Liaoning, China,Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, Liaoning, China,Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, Liaoning, China,Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, Liaoning, China,Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, Liaoning, China and Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, Liaoning, China
Abstract:
Keywords:Jarud Basin  Late Jurassic  rhyolites  Manketouebo Formation  zircon U-Pb dating  Hf isotope
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