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贺根山缝合带白音呼舒奥长花岗岩锆石U-Pb年龄、地球化学特征及构造意义
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  • 英文篇名:Zircon U-Pb ages and geochemical characteristics of Baiyinhushu trondhjemite in Hegenshan suture zone and their tectonic implications
  • 作者:王金芳 ; 李英杰 ; 李红阳 ; 董培培
  • 英文作者:WANG Jinfang;LI Yingjie;LI Hongyang;DONG Peipei;School of Nature Resources,Hebei Geo University;
  • 关键词:英云闪长岩—奥长花岗岩—花岗闪长岩(Tonalite—Trondhjemite—Granodiorite ; TTG)岩系 ; 岛弧岩浆岩 ; 晚石炭世 ; 锆石U-Pb年代学 ; 二连—贺根山缝合带
  • 英文关键词:Trondhjemite;;Tonalite—Trondhjemite—Granodiorite series,TTG series;;arc magmatic rocks;;Late Carboniferous;;zircon U-Pb geochronology;;Erenhot—Hegenshan (Hegen Mountains) suture zone
  • 中文刊名:地质论评
  • 英文刊名:Geological Review
  • 机构:河北地质大学资源学院;
  • 出版日期:2019-07-15
  • 出版单位:地质论评
  • 年:2019
  • 期:04
  • 基金:国家自然科学基金资助项目“内蒙古西乌旗迪彦庙蛇绿岩年代学、地球化学及大地构造意义”(编号:41502211);; 中国地质调查局项目“内蒙古1∶5万高力罕牧场三连等四幅区调”(编号:1212011120711),“内蒙古1∶5万沙日勒昭等四幅区调”(编号:1212011120701)的成果~~
  • 语种:中文;
  • 页:79-94
  • 页数:16
  • CN:11-1952/P
  • ISSN:0371-5736
  • 分类号:P588.121;P597.3
摘要
本文以出露于贺根山缝合带梅劳特乌拉蛇绿岩北侧的白音呼舒奥长花岗岩体为研究对象,通过野外地质调查和岩石学、地球化学、锆石LA-ICP-MS U-Pb年代学研究,探讨其成因、构造环境及二连—贺根山洋俯冲消亡过程。岩石地球化学研究表明,白音呼舒岩体富硅(SiO_2=66.50%~73.04%)、高铝(Al_2O_3=15.11%~16.75%)、富钠(Na_2O=3.50%~6.16%)、低钾(K_2O=1.46%~2.38%),相对高锶(Sr=167.0×10~(-6)~441.0×10~(-6))、低钇(Y=5.30×10~(-6)~9.51×10~(-6)),富集Ba、Sr等大离子亲石元素和LREE,亏损Nb、Ta、Ti、P等高场强元素和HREE,无明显Eu异常。岩石学和岩石地球化学特征表明,白音呼舒侵入岩体属于英云闪长岩—奥长花岗岩—花岗闪长岩(Tonalite—Trondhjemite—Granodiorite,TTG)岩系,与高Si高锶低钇中酸性岩(Adakite,埃达克岩)类似,形成于大洋俯冲带岛弧环境,为俯冲洋壳脱水熔融的产物。锆石LA-ICP-MS U-Pb测年表明,白音呼舒奥长花岗岩体的形成年龄为309.2±1.6 Ma,表明该岩体侵位于晚石炭世,反映了贺根山缝合带晚石炭世大洋俯冲带TTG岩浆作用事件。结合二连—贺根山缝合带石炭纪蛇绿岩、石炭纪—二叠纪岛弧型岩浆岩和中生代后造山A型岩浆岩的时空分布与演化关系,表明古亚洲洋二连—贺根山洋盆在晚石炭世并未关闭,而是处于大洋俯冲消减和陆壳增生过程中。
        Objectives: The Baiyinhushu trondhjemite(belongs to Tonalite—Trondhjemite—Granodiorite series,TTG series) is newly identified in the Meilaotewula SSZ(Supra Subduction Zone)-type ophiolite of the Hegenshan(Hegen Mountains) suture zone,Inner Mongolia. TTGs are usually believed to result from the dehydration melting of subducted oceanic crust,to represent oceanic subduction and juvenile continental growth. However,whether the Late Carboniferous Paleo—Asian Ocean was still in subduction stage lacks further definitely petrological and chronological evidence and constraints. Therefore,this study carried out zircon LA-ICP-MS U-Pb geochronology and geochemistry on the Baiyinhushu TTG to discuss its origin,in order to provide new evidence for the tectonic evolution of the Hegenshan suture zone of the eastern Central Asian Orogenic Belt.Methods: Based on field geological surveying, petrology, geochemistry and LA-ICP-MS zircon U-Pb geochronology of the Baiyinhushu trondhjemite,this paper discusses the petrogenesis and tectonic setting of the trondhjemite,and the final closure time and subduction process of the Paleo—Asian Ocean.Results: The trondhjemite has high SiO_2(66.50% ~ 73.04%),Al_2O_3(15.11% ~ 16.75%),Na_2O(3.50% ~6.16%),Sr(167.0×10~(-6)~ 441.0 × 10~(-6)) and low K_2O(1.46% ~ 2.38%),Y(5.30 × 10~(-6)~ 9.51 × 10~(-6)) contents,enriched in Ba,Sr large ion lithophile elements and LREE,and depleted in Nb,Ta,Ti,P high field strength elements and HREE. There is no pronounced Eu anomaly. The Baiyinhushu pluton belongs to high-Al TTG rocks and is similar to high-SiO_2 adakites. The zircon U-Pb LA-ICP-MS dating shows that the Baiyinhushu pluton was formed at 309.2 ± 1.6 Ma,indicating that the pluton emplaced in the Late Carboniferous,reflecting the TTG magmatism and juvenile continental growth of oceanic subduction zone in the Hegenshan suture at the Late Carboniferous.Conclusions: This study determines the Late Carboniferous(309.2 ± 1.6 Ma) Baiyinhushu TTG,which was probably formed in island—arc setting of oceanic subduction zone and is arc magmatic rocks. The TTG might have been derived from the dehydration melting of subducted oceanic crust. The discovery and confirmation of the Baiyinhushu TTG in the Late Carboniferous provide new evidence for Paleo—Asian Ocean subduction and juvenile continental growth.
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