岩矿测试

文章摘要

谢奋全,王黎栋,李琦,石朝霞,陈学兵,韦岸.阿拉善宗乃山岩体东南缘花岗岩LA-ICP-MS锆石U-Pb年龄与地球化学特征[J].岩矿测试,2015,34(3):375-382

XIE Fen-quan,WANG Li-dong,LI Qi,SHI Zhao-xia,CHEN Xue-bing,WEI An.Zircon LA-ICP-MS Dating of Granites from the Southeastern Zongnai Mountain Alax and Its Geochemical Characteristics[J].Rock and Mineral Analysis,2015,34(3):375-382.DOI:10.15898/j.cnki.11-2131/td.2015.03.019

阿拉善宗乃山岩体东南缘花岗岩LA-ICP-MS锆石U-Pb年龄与地球化学特征

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Zircon LA-ICP-MS Dating of Granites from the Southeastern Zongnai Mountain Alax and Its Geochemical Characteristics

投稿时间：2014-03-16 修订日期：2015-05-10

DOI：10.15898/j.cnki.11-2131/td.2015.03.019

中文关键词: 阿拉善宗乃山岩体花岗岩锆石U-Pb年龄地球化学特征

英文关键词: the Zongnai mountain rocks in alxa granite, the U-Pb ages of zircon geochemical characteristics

基金项目:国防科工局高放废物地质处置研究开发项目(内蒙阿拉善高放废物地质处置备选场址预选及评价研究“内蒙阿拉善地区主要构造岩浆系统特征及地球动力学背景”课题)

作者	单位
谢奋全	中国地质大学(北京)水资源与环境学院, 北京 100083
王黎栋	中国地质大学(北京)水资源与环境学院, 北京 100083
李琦	中国地质大学(北京)海洋学院, 北京 100083
石朝霞	燕山大学教务处, 河北秦皇岛 066004
陈学兵	中国地质大学(北京)水资源与环境学院, 北京 100083
韦岸	中国地质大学(北京)海洋学院, 北京 100083

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中文摘要:

阿拉善宗乃山岩体东南缘分布多种类型的花岗岩,本文主要采用岩相学、激光剥蚀电感耦合等离子体质谱(LA-ICP-MS)锆石U-Pb定年、岩石地球化学等技术手段, 对宗乃山岩体东南缘岩石类型、年代学、源岩特征以及构造背景进行了研究。结果表明:岩石类型主要为碱性-钙碱性准铝质花岗岩和闪长岩;单颗粒锆石分析获得黑云母斜长花岗岩年龄为236.8±1.9 Ma~249.7±2.6 Ma, 片麻状花岗岩年龄为268.1±1.1 Ma, 岩体成岩时期主要为华力西晚期和印支期早期, 具有多期侵入的特征。该岩体岩石源岩为I型花岗岩, 源于地壳火山弧区和同碰撞区, 表明由于洋壳俯冲作用, 在宗乃山东南缘形成了岛弧花岗岩侵入体。LA-ICP-MS锆石U-Pb定年技术为洋壳俯冲提供了年代学约束, 确定了研究区碰撞时间为早于236.8±1.9 Ma。

英文摘要:

There are many types of granites around the southeastern Zongnai Mountain rock mass in Alax, the types of rocks, the characteristics of source rocks, and tectonic setting by using the LA-ICP-MS zircon geochronology, petrographic observation, geochemical methods (major, trace and REE elements) of granites and diorites from southeastern Zongnai Mountain rock in Alax are discussed. The rocks are mainly alkaline-calc-alkaline metaluminous granites and diorites. LA-ICP-MS zircon U-Pb dating yielded ages of 236.6±0.95 Ma to 249.7±2.6 Ma for the plagioclase and biotite granite and 268.4±0.69 Ma for the gneissic granite. Therefore, these rocks were formed mainly during the late Variscan and early Indosinian periods and are characteristic of multi-stage intrusions. The values of TiO₂, A/CNK, A/NK, 10000*Ga/Al, etc. and the abnormal elements Ba, Ta, Sr, Eu, etc. indicate that these granites are I-type granites. Major, trace and rare earth elements indicate that these rock are mainly derived from volcanic arc crust and locally derived from the collision zone. Due to the subduction of oceanic crust in the southeastern Zongnai mountain, arc margin orogenic granite intrusions and other variations were formed with continental margin arc characteristics. LA-ICP-MS zircon ages provide timing constraints for the subducted oceanic crust and conclude that the collision time is earlier than 236.8±1.9 Ma.

主管单位：	中国科学技术协会
主办单位：	中国地质学会岩矿测试技术专业委员会国家地质实验测试中心