内蒙古西乌珠穆沁旗晚二叠世花岗岩的锆石U-Pb年龄、地球化学特征及其构造意义
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摘要
西乌珠穆沁旗西南部色尔崩岩体和努和亭沙拉岩体的锆石U-Pb年龄为255. 3±1. 4 Ma和254. 4±3. 4 Ma,是晚二叠世晚期岩浆活动的产物。岩石地球化学分析发现,花岗岩属于钙碱系列,富钠贫钾,具有高Sr(Sr≥741×10~(-6))低Y、Yb及高Sr/Y的特点,轻重稀土分异显著(10. 25<(La/Yb)_N<22. 51),弱的正Eu异常(1. 06 <δEu <1. 46),富集大离子亲石元素(LILE),亏损高场强元素(HFSE),与典型的高锶低钇中酸性岩(adakite,亦有人译为埃达克岩)地球化学特征相似。岩浆锆石具有正的ε_(Hf)(t)值(+8. 1～+13. 3)和年轻的二阶段模式年龄(T_(2DM)约为430～760 Ma),高Mg~#(55～59),表明岩浆熔体与地幔橄榄岩发生了相互作用,暗示这种高锶低钇型花岗岩的形成与俯冲板片在深部发生部分熔融有关。结合区域地质资料认为,古亚洲洋在晚二叠世还未完全闭合,研究区内高锶低钇型花岗岩形成于古亚洲洋持续向北俯冲且俯冲洋壳断离并发生部分熔融构造背景下。
Objectives: Adakite is a kind of intermediate—acid rock with unique geochemical characteristics. It can track the oceanic crust subduction and crustal thickening and other related events in geological history,which is of great significance for the inversion of crustal composition and mineralization. According to previous studies,the granites of Seerbeng and Nuhetingshala in West Ujimqin have the characteristics of adakite,but lacked accurate chronology data. The study on the diagenetic age and tectonic background of the adakite granitoids is helpful to understand the tectonic evolution of the paleo-Asian Ocean.Methods: Based on the field work,through the microscope observation,the whole rock chemical analysis,LAICP-MS U-Pb zircon dating of the granitiods and the Hf isotopic analysis.Results: The U-Pb isotopic dating of zircon shows that the ages of Seerbeng pluton and Nuhetingshala pluton in West Ujimqin area are 255.3±0.7 Ma and 254.4±1.2 Ma,which are the products of magmatic activity in the late Permian.By lithology and rock geochemistry analysis found that belong to calc-alkalic rock and high potassium calcalkali series,SiO2 content is 65% ～ 73%,Na-rich and K-poor,high Sr,low Yb Y and high Sr/Y,wich consistent with the characteristics of typical adakite.The magmatic zircons are positively εHf( t) values( + 8.1 ～ + 13.3) and young two-stage model ages varied in 430 ～ 760 Ma. Adakite rock formation is related to partial melting of young subduction plate,and the high Mg#indicates that magmatic melts interact with mantle peridotite.Conclusions: Combined with regional rock assemblages,the paleo-Asian Ocean has not yet completely closed in late Permian. During this stage,the subducted oceanic crust broke off and partially melted,which formed the adakite granitoids and hight-Mg andesite. The closing time of the paleo-Asian ocean should be after the Permian.
Objectives: Adakite is a kind of intermediate—acid rock with unique geochemical characteristics. It can track the oceanic crust subduction and crustal thickening and other related events in geological history,which is of great significance for the inversion of crustal composition and mineralization. According to previous studies,the granites of Seerbeng and Nuhetingshala in West Ujimqin have the characteristics of adakite,but lacked accurate chronology data. The study on the diagenetic age and tectonic background of the adakite granitoids is helpful to understand the tectonic evolution of the paleo-Asian Ocean.Methods: Based on the field work,through the microscope observation,the whole rock chemical analysis,LAICP-MS U-Pb zircon dating of the granitiods and the Hf isotopic analysis.Results: The U-Pb isotopic dating of zircon shows that the ages of Seerbeng pluton and Nuhetingshala pluton in West Ujimqin area are 255.3±0.7 Ma and 254.4±1.2 Ma,which are the products of magmatic activity in the late Permian.By lithology and rock geochemistry analysis found that belong to calc-alkalic rock and high potassium calcalkali series,SiO2 content is 65% ～ 73%,Na-rich and K-poor,high Sr,low Yb Y and high Sr/Y,wich consistent with the characteristics of typical adakite.The magmatic zircons are positively εHf( t) values( + 8.1 ～ + 13.3) and young two-stage model ages varied in 430 ～ 760 Ma. Adakite rock formation is related to partial melting of young subduction plate,and the high Mg#indicates that magmatic melts interact with mantle peridotite.Conclusions: Combined with regional rock assemblages,the paleo-Asian Ocean has not yet completely closed in late Permian. During this stage,the subducted oceanic crust broke off and partially melted,which formed the adakite granitoids and hight-Mg andesite. The closing time of the paleo-Asian ocean should be after the Permian.
引文
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