新疆阿尔泰山西段乞格拉塔乌岩体LA-ICP-MS锆石U-Pb同位素年龄及其地质意义
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摘要
新疆阿尔泰山西段发育的花岗岩体缺乏精确地锆石U-Pb同位素年龄资料。本次在乞格拉塔乌岩体中获得了425.1±4.4Ma的LA-ICP-MS锆石U-Pb同位素年龄数据,将其形成时代厘定为中志留世。岩石SiO_2含量在64.07%～73.77%之间,Al_2O_3含量为12.40%～15.71%, A/CNK值为1.02～1.10,全碱(ALK)含量为5.85%～7.93%,里特曼指数(σ)为1.62～2.24,具有弱过铝质、高钾钙碱性系列花岗岩特征;稀土总量介于166.3×10~(-6)～197.2×10~(-6)之间,轻、重稀土分馏明显,δEu值介于0.47～0.63之间,具明显负Eu异常。微量元素富集Rb、Th、U等大离子亲石元素及La、Ce、Sm等,亏损Nb、Zr等高场强元素及Sr、P、Ti等,具有低Sr高Yb的特征(Sr含量在93.7×10~(-6)～211×10~(-6),Yb含量在2.1×10~(-6)～3.9×10~(-6))。研究表明,古亚洲洋从奥陶纪开始向北俯冲,一直持续到晚古生代中晚期。早古生代末期形成的乞格拉塔乌岩体,既有俯冲环境特征,又显示了后碰撞花岗岩类特点,其复杂的成因可能与古亚洲洋存在洋中脊俯冲作用有关。
Objectives: The magmatic activity were well active in western Altay Mountains,the Northern of Xinjiang,but the high precision LA-ICP-MS zircon U-Pb geochronological data of the granitoids is absent. In this work,LA-ICPMS zircon U-Pb geochronological and geochemical samples of the Qigelatawu intrusive rocks were collected to study the magmatic activity and tectonic evolution information of the Altay orogenic belt.Methods: Based on LA-ICP-MS zircon U-Pb isotope dating,defining the formation age of the Qigelatawu intrusion,and using geochemical data of the intrusive rocks to distinguish the magmatic genesis and tectonic environment of the Altay orogenic belt.Results: The LA-ICP-MS zircon U-Pb age(206 Pb/238 U weighted average age) of the Qigelatawu intrusive rocks is 425.1±4.4 Ma,revealed that the intrusive rocks formed in the Middle Silurian. The SiO_2 content ranges from 64.07% to 73.77%,Al_2 O_3 content range from 12. 4% to 15. 71% and A/CNK ranges between 0. 88 ～ 1. 16,ALK ranges between 5.85% ～ 7.93% and σ from 1. 62 to 2. 24,with wearly per-aluminous,high-K calc-alkaline series rocks. The content of REE ranges between 166. 28 × 10~(-6)～ 197. 22 × 10~(-6),light—heavy REEs fractionation strong,Eu negative anomalies( δEu = 0.47 ～ 0.63). The geochemical characteristics of the pluton are that trace elements are enriched in Rb,Th,U( LILE) and La,Ce,Sm,etc.,poored in Nb,Zr( HFSE) and Sr,P,Ti,etc.,low in Sr and high in Yb( Sr ranges between 93.7 × 10~(-6)～ 211 × 10~(-6),Yb ranges between 2.1×10~(-6)～ 3.9 ×10~(-6)). This study demonstrated that the Qigelatawu intrusion has the characteristics of subduction environment and shows the characteristics of post-collision granites.Conclusions: Research shows that ancient Asian Ocean subducted north from the Ordovician and continued until the late Middle Paleozoic. The Qigelatawu intrusive rocks,which formed at the end of Early Paleozoic,its complex causes may be related to the ridge subduction in the ancient Asian Ocean.
Objectives: The magmatic activity were well active in western Altay Mountains,the Northern of Xinjiang,but the high precision LA-ICP-MS zircon U-Pb geochronological data of the granitoids is absent. In this work,LA-ICPMS zircon U-Pb geochronological and geochemical samples of the Qigelatawu intrusive rocks were collected to study the magmatic activity and tectonic evolution information of the Altay orogenic belt.Methods: Based on LA-ICP-MS zircon U-Pb isotope dating,defining the formation age of the Qigelatawu intrusion,and using geochemical data of the intrusive rocks to distinguish the magmatic genesis and tectonic environment of the Altay orogenic belt.Results: The LA-ICP-MS zircon U-Pb age(206 Pb/238 U weighted average age) of the Qigelatawu intrusive rocks is 425.1±4.4 Ma,revealed that the intrusive rocks formed in the Middle Silurian. The SiO_2 content ranges from 64.07% to 73.77%,Al_2 O_3 content range from 12. 4% to 15. 71% and A/CNK ranges between 0. 88 ～ 1. 16,ALK ranges between 5.85% ～ 7.93% and σ from 1. 62 to 2. 24,with wearly per-aluminous,high-K calc-alkaline series rocks. The content of REE ranges between 166. 28 × 10~(-6)～ 197. 22 × 10~(-6),light—heavy REEs fractionation strong,Eu negative anomalies( δEu = 0.47 ～ 0.63). The geochemical characteristics of the pluton are that trace elements are enriched in Rb,Th,U( LILE) and La,Ce,Sm,etc.,poored in Nb,Zr( HFSE) and Sr,P,Ti,etc.,low in Sr and high in Yb( Sr ranges between 93.7 × 10~(-6)～ 211 × 10~(-6),Yb ranges between 2.1×10~(-6)～ 3.9 ×10~(-6)). This study demonstrated that the Qigelatawu intrusion has the characteristics of subduction environment and shows the characteristics of post-collision granites.Conclusions: Research shows that ancient Asian Ocean subducted north from the Ordovician and continued until the late Middle Paleozoic. The Qigelatawu intrusive rocks,which formed at the end of Early Paleozoic,its complex causes may be related to the ridge subduction in the ancient Asian Ocean.
引文
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