阿尔泰造山带南缘库尔提地区寒武纪变质侵入体的发现及地质意义

张亚峰, 蔺新望, 王煜, 陈宁, 王星, 郭岐明, 赵端昌, 吕军利. 阿尔泰造山带南缘库尔提地区寒武纪变质侵入体的发现及地质意义[J]. 西北地质, 2015, 48(3): 271-279.
引用本文: 张亚峰, 蔺新望, 王煜, 陈宁, 王星, 郭岐明, 赵端昌, 吕军利. 阿尔泰造山带南缘库尔提地区寒武纪变质侵入体的发现及地质意义[J]. 西北地质, 2015, 48(3): 271-279.
ZHANG Yafeng, LIN Xinwang, WANG Yu, CHEN Ning, WANG Xing, GUO Qiming, ZHAO Duanchang, LV Junli. Discovery and Geological Significance of Cambrian Metamorphic Intrusions of Kuerti Region in Southern Altay Orogenic Belt[J]. Northwestern Geology, 2015, 48(3): 271-279.
Citation: ZHANG Yafeng, LIN Xinwang, WANG Yu, CHEN Ning, WANG Xing, GUO Qiming, ZHAO Duanchang, LV Junli. Discovery and Geological Significance of Cambrian Metamorphic Intrusions of Kuerti Region in Southern Altay Orogenic Belt[J]. Northwestern Geology, 2015, 48(3): 271-279.

阿尔泰造山带南缘库尔提地区寒武纪变质侵入体的发现及地质意义

  • 基金项目: 中国地质调查局区域地质调查“新疆1:25万可可托海、江德勒克幅区调修测”(1212011120503)、“新疆青河县1:5万阿克布拉克、阿尔沙特、昆格依特、喀拉布腊乌幅区调”(1212011120509)共同资助

Discovery and Geological Significance of Cambrian Metamorphic Intrusions of Kuerti Region in Southern Altay Orogenic Belt

  • 在新疆富蕴县库尔提地区下元古界克木齐岩群中发现了一套变质侵入体, 并对其进行了LA-ICP-MS锆石UVPb同位素定年。根据锆石的阴极发光图像和Th、U含量等特征, 锆石可分为岩浆锆石、变质锆石和捕获锆石3类。测得片麻岩的原岩岩浆206Pb/238U加权平均年龄为(496.3±6.4) Ma(MSWD = 0.74), 变质年龄介于444~452Ma之间。结合区域地质资料, 前者可能代表了古亚洲洋向北起始俯冲的时限, 后者代表同造山期变质事件时代。同时, 研究中发现的捕获继承性岩浆锆石年龄为783~901Ma, 暗示阿尔泰造山带存在前寒武纪基底。
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收稿日期:  2015-04-15
修回日期:  2015-05-20
刊出日期:  2015-09-15

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