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现代地质 ›› 2017, Vol. 31 ›› Issue (06): 1170-1176.

• 岩石学 • 上一篇    下一篇

北祁连缝合带油葫芦沟蛇绿岩中花岗斑岩锆石U-Pb年龄及地质意义

李冰1,2(), 胡道功2(), 陈宣华1, 张耀玲2, 吴环环2, 王超群2   

  1. 1.中国地质科学院 地球深部探测中心,北京 100037
    2.中国地质科学院 地质力学研究所,北京 100081
  • 收稿日期:2016-03-21 修回日期:2016-11-20 出版日期:2017-12-10 发布日期:2017-12-25
  • 通讯作者: 胡道功,男,研究员,博士,1963年出生,构造地质学专业,主要从事新构造与活动构造研究。Email:hudg@263.net
  • 作者简介:李 冰,男,助理研究员,博士研究生,1987年出生,构造地质学专业,主要从事青藏高原东北缘构造地质研究。Email:libing@cags.ac.cn
  • 基金资助:
    中国地质调查局项目“祁连-天山及周缘盆山结合带深部地质调查”(DD20160083);“中国及邻区成矿构造背景编图研究”(DD20160344)

Zircon U-Pb Age of Granite Porphyry Within Youhulugou Ophiolite in the Suture Zone of North Qilian Mountains and Its Geological Implications

LI Bing1,2(), HU Daogong2(), CHEN Xuanhua1, ZHANG Yaoling2, WU Huanhuan2, WANG Chaoqun2   

  1. 1. SinoProbe Centre, Chinese Academy of Geological Sciences,Beijing 100037,China
    2. Institute of Geomechanics, Chinese Academy of Geological Sciences,Beijing 100081,China
  • Received:2016-03-21 Revised:2016-11-20 Online:2017-12-10 Published:2017-12-25

摘要:

蛇绿岩是保存在陆或弧上的大洋岩石圈残片,是洋中脊扩张或板块俯冲消减过程的产物。花岗质岩石可存在于蛇绿岩形成的不同阶段,是研究蛇绿岩形成演化和精确定年的重要岩石单元。油葫芦沟蛇绿岩是北祁连缝合带中具有代表性的蛇绿岩残片之一,对侵入到玄武岩中的花岗斑岩进行地球化学分析,结果表明花岗斑岩具有过铝和高钾特征,稀土和微量元素表现出明显的LREE富集,具有典型的仰冲型花岗岩特征。对花岗斑岩进行LA-ICP-MS锆石U-Pb测年,20个测点数据的206Pb/238U加权平均年龄为(497.5±1.5) Ma,该年龄代表了花岗斑岩的形成年龄及蛇绿岩仰冲就位的时代。结合北祁连蛇绿岩带的地质概况、年龄数据和地球化学特征,认为油葫芦沟蛇绿岩在晚寒武世仰冲就位,为北祁连洋向北俯冲提供了重要的时间约束。

关键词: 北祁连缝合带, 油葫芦沟蛇绿岩, 仰冲型花岗斑岩, 锆石U-Pb年龄

Abstract:

Ophiolites as on-land or arc slices of oceanic lithosphere, are the production of the mid ocean ridge expansion or subduction of the plates. The granitoids can be formed during the formation of ophiolites and are important for studying origin of the ophiolites, especially dating the precise ages of the ophiolites formation and evolution. The Youhulugou ophiolite is one of the representative ophiolite fragments in the suture zone of the North Qilian Mountain. In this study, major and trace elements geochemical study indicates that the granite porphyry within Youhulugou ophiolite has high Al2O3 and K2O content characteristics. According to the moderate LREE-enrichment patterns, the granite porphyry is similar to the obduction-type granitoids rocks within ophiolites. LA-ICP-MS U-Pb dating was carried out for zircons from isotropic granite porphyry within Youhulugou ophiolite. Twenty point analyses yield a relatively consistent and apparent 206Pb/238U weighted mean age of (497.5±1.5) Ma, which is considered to be the forming age of the granite porphyry and the obduction age of the Youhulugou ophiolite onto the continental crust. Combined with regional geological characteristics, chronological and geochemical data,we concluded that the Youhulugou ophiolite obducted during the Late Cambrian era, and the acquisition of forming age and determination of tectonic setting for Youhulugou ophiolite provide significant constraints on the age of intra-oceanic subduction system in the North Qilian Ocean.

Key words: North Qilian suture zone, Youhulugou ophiolite, obduction-type granite porphyry, zircon U-Pb age

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