三江造山带北段扎河岩体锆石LA-ICP-MS U-Pb年龄及其地质意义

马俊强, 张运昌, 陈根, 纪国忠, 廖强, 杨晓君. 三江造山带北段扎河岩体锆石LA-ICP-MS U-Pb年龄及其地质意义[J]. 西北地质, 2017, 50(4): 70-80.
引用本文: 马俊强, 张运昌, 陈根, 纪国忠, 廖强, 杨晓君. 三江造山带北段扎河岩体锆石LA-ICP-MS U-Pb年龄及其地质意义[J]. 西北地质, 2017, 50(4): 70-80.
MA Junqiang, ZHANG Yunchang, CHEN Gen, JI Guozhong, LIAO Qiang, YANG Xiaojun. LA-ICP-MS Zircon U-Pb Ages of the Zhahe Pluton in North Part of Sanjiang Orogenic Belt and Its Geological Significance[J]. Northwestern Geology, 2017, 50(4): 70-80.
Citation: MA Junqiang, ZHANG Yunchang, CHEN Gen, JI Guozhong, LIAO Qiang, YANG Xiaojun. LA-ICP-MS Zircon U-Pb Ages of the Zhahe Pluton in North Part of Sanjiang Orogenic Belt and Its Geological Significance[J]. Northwestern Geology, 2017, 50(4): 70-80.

三江造山带北段扎河岩体锆石LA-ICP-MS U-Pb年龄及其地质意义

  • 基金项目: 中国地质调查局地质调查项目“青海省治多县俄昌公仁地区1:5万I46E012020、I46E013020、I46E014020三幅区域地质矿产调查”项目(12120113033500)

LA-ICP-MS Zircon U-Pb Ages of the Zhahe Pluton in North Part of Sanjiang Orogenic Belt and Its Geological Significance

  • 扎河岩体产出于三江造山带北段可可西里-金沙江缝合带,呈北西向展布,受北西向断裂构造控制。笔者通过详细调查,在石英闪长岩锆石中获得的(190.4±2.8)Ma的年龄值,在富石英英云闪长岩锆石中获得的(192.1±1.2)Ma的年龄值,基本反映了扎河岩体成岩于早侏罗世,表明金沙江结合带经受了该时期构造-岩浆活动的影响。稀土元素特征表明该套侵入岩属轻稀土富集、重稀土平坦型,具有弱正Eu异常,反映岩石经历了一定程度的分离结晶作用,微量元素显示出活动大陆边缘岛弧岩浆的特征,笔者通过野外地质调查,结合区域构造演化,认为侏罗纪早期三江北段已进入碰撞后陆内汇聚阶段,该期构造-岩浆事件的发生是受班公湖-怒江洋向北俯冲消减持续影响效应的产物。
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出版历程
收稿日期:  2016-12-03
修回日期:  2017-08-04
刊出日期:  2017-12-15

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