| 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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| 引用本文： | 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. |
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| 作者姓名： | 谢奋全 王黎栋 李琦 石朝霞 陈学兵 韦岸 |
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| 作者单位： | 中国地质大学(北京)水资源与环境学院, 北京 100083,中国地质大学(北京)水资源与环境学院, 北京 100083,中国地质大学(北京)海洋学院, 北京 100083,燕山大学教务处, 河北 秦皇岛 066004,中国地质大学(北京)水资源与环境学院, 北京 100083,中国地质大学(北京)海洋学院, 北京 100083 |
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| 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) |
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| 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。
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| 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 |
| 收稿时间： | 2014/3/16 0:00:00 |
| 修稿时间： | 2015/5/10 0:00:00 |
Zircon LA-ICP-MS Dating of Granites from the Southeastern Zongnai Mountain Alax and Its Geochemical Characteristics |
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| XIE Fen-quan,WANG Li-dong,LI Qi,SHI Zhao-xi,CHEN Xue-bing and 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. |
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| Authors: | XIE Fen-quan WANG Li-dong LI Qi SHI Zhao-xi CHEN Xue-bing and WEI An |
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| Institution: | School of Water Resource and Environment, China University of Geosciences (Beijing), Beijing 100083, China,School of Water Resource and Environment, China University of Geosciences (Beijing), Beijing 100083, China,School of Ocean Sciences, China University of Geosciences (Beijing), Beijing 100083, China,Office of Academic Affairs, Yanshan University, Qinhuangdao 066004, China,School of Water Resource and Environment, China University of Geosciences (Beijing), Beijing 100083, China and School of Ocean Sciences, China University of Geosciences (Beijing), Beijing 100083, China |
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| Abstract: | 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. |
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| Keywords: | the Zongnai mountain rocks in alxa granite the U-Pb ages of zircon geochemical characteristics |
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