藏南冈底斯带中段早侏罗世岩浆作用的厘定及其大地构造意义
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摘要
以藏南冈底斯带中段的东嘎花岗岩体和奴玛花岗岩体为研究对象,对其进行了锆石U-Pb年代学、Lu-Hf同位素和全岩地球化学综合分析,据此探讨其岩石成因和大地构造意义。东嘎花岗岩体主要由石英、长石以及少量黑云母、角闪石组成;奴玛花岗岩体主要由石英、长石以及少量黑云母组成。锆石LA-ICP-MS U-Pb定年结果显示,东嘎花岗岩体的加权平均年龄为185.8±2.3 Ma,奴玛花岗岩体的加权平均年龄为185.9±2.2Ma和185.1±1.7 Ma,两个岩体具有一致的成岩年龄,为同一期岩浆事件的产物。在地球化学组成上,两个岩体均富集轻稀土(LREE)和大离子亲石元素(LILE),亏损Nb、Ta、Ti等高场强元素(HFSE),具有明显的俯冲带岩浆岩特征;里特曼指数和铝饱和指数显示,两个岩体属于弱过铝质钙碱性I型花岗岩。锆石Lu-Hf结果显示,两个岩体均具有显著亏损的锆石Hf同位素组成和极高的εHf(t)值(分别为+11.14~+15.55,平均值+13.76;+9.49~+15.52,平均值+13.56)以及相对年轻的二阶段模式年龄(T_(DM2)),反映了它们的源区以新生地壳的部分熔融为主。综合研究表明:早侏罗世(普林斯巴期)时,藏南冈底斯地区应为典型的活动大陆边缘环境,花岗质岩石的形成和新特提斯洋向拉萨地体的北向俯冲有关,其成因与幔源岩浆的底侵引起新生下地壳的部分熔融有关。
In this paper,we conducted systematically zircon LA-ICP-MS U-Pb dating,Lu-Hf isotopic analyses and whole-rock geochemical analyses for two granitic plutons(Donggagranitic pluton and Numa granitic pluton),and elucidated their petrogenesis and tectonic setting in the middle Gangdese batholith,southern Tibet.The Donggagranitic pluton is mainly composed of quartz and feldspar,with minor amount of biotite and hornblende.The Numa granitic pluton consists of quartz and feldspar dominantly as well as minor amount of biotite.The zircon U-Pb dating yielded a mean age of 185.8±2.3 Ma for the Dongga pluton and two mean ages of 185.9±2.2 Ma and 185.1±1.7 Ma for the Numa pluton.The results show the similar diagenesis ages,indicating they were the products of the simultaneous magmatic event in the Gangdese batholith,southern Tibet.Geochemically,two granitic plutons show enrichment of LREE and LILE as well as depletions of HFSE(Nb,Ta and Ti),suggesting a subduction-related tectonic setting.Rittmann and Aluminium saturation signatures suggest that those two granitic plutons belong to typical calc-alkaline and weak peraluminous(A/CNK)I-type granite.Zircon Hf isotopic components demonstrate that the Dognga and Numa plutons are characterized by highly depleted Hf isotopic compositions and young second model ages(t_(DM2)),with theεHf(t)values of+11.14～+15.55(mean value+13.76)and+9.49～+15.52(mean value +13.56),respectively,indicating that the granitic plutons originated from partial melting of juvenile crustal materials.During the partial melting,underplating mantle magma played a key role in causing the partial melting of the lower crustal juvenile materials in the Gangdese belt.Integrated study,along with previous studied results,indicates that the granitic plutons were generated in an active continental margin arc setting related to the northward subduction of the Neo-Tethys oceanic crust beneath the Lhasa terrane during the Early Jurassic(Pliensbachian stage)in the Gangdese belt,southern Tibet.
In this paper,we conducted systematically zircon LA-ICP-MS U-Pb dating,Lu-Hf isotopic analyses and whole-rock geochemical analyses for two granitic plutons(Donggagranitic pluton and Numa granitic pluton),and elucidated their petrogenesis and tectonic setting in the middle Gangdese batholith,southern Tibet.The Donggagranitic pluton is mainly composed of quartz and feldspar,with minor amount of biotite and hornblende.The Numa granitic pluton consists of quartz and feldspar dominantly as well as minor amount of biotite.The zircon U-Pb dating yielded a mean age of 185.8±2.3 Ma for the Dongga pluton and two mean ages of 185.9±2.2 Ma and 185.1±1.7 Ma for the Numa pluton.The results show the similar diagenesis ages,indicating they were the products of the simultaneous magmatic event in the Gangdese batholith,southern Tibet.Geochemically,two granitic plutons show enrichment of LREE and LILE as well as depletions of HFSE(Nb,Ta and Ti),suggesting a subduction-related tectonic setting.Rittmann and Aluminium saturation signatures suggest that those two granitic plutons belong to typical calc-alkaline and weak peraluminous(A/CNK)I-type granite.Zircon Hf isotopic components demonstrate that the Dognga and Numa plutons are characterized by highly depleted Hf isotopic compositions and young second model ages(t_(DM2)),with theεHf(t)values of+11.14～+15.55(mean value+13.76)and+9.49～+15.52(mean value +13.56),respectively,indicating that the granitic plutons originated from partial melting of juvenile crustal materials.During the partial melting,underplating mantle magma played a key role in causing the partial melting of the lower crustal juvenile materials in the Gangdese belt.Integrated study,along with previous studied results,indicates that the granitic plutons were generated in an active continental margin arc setting related to the northward subduction of the Neo-Tethys oceanic crust beneath the Lhasa terrane during the Early Jurassic(Pliensbachian stage)in the Gangdese belt,southern Tibet.
引文
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