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现代地质 ›› 2018, Vol. 32 ›› Issue (02): 329-334.DOI: 10.19657/j.geoscience.1000-8527.2018.02.11

• 岩石学 • 上一篇    下一篇

柴北缘牦牛山组火山岩锆石U-Pb年龄及其地质意义

张耀玲1,2(), 倪晋宇3, 沈燕绪4, 王超群2, 高万里2, 胡道功2   

  1. 1.中国地质大学(北京) 地球科学与资源学院,北京 100083
    2.中国地质科学院 地质力学研究所,北京 100081
    3.中国五矿集团公司 五矿勘查开发有限公司,北京 100010
    4.国土资源实物地质资料中心,河北 廊坊 065201
  • 收稿日期:2017-07-23 修回日期:2017-12-01 出版日期:2018-04-10 发布日期:2018-05-07
  • 作者简介:张耀玲,女,助理研究员,博士研究生,1984年出生,矿物学、岩石学、矿床学专业,主要从事火山岩与新构造研究。Email:yaoling_zhang@126.com
  • 基金资助:
    中国地质调查局柴达木盆地及周缘油气基础地质调查子项目(121201104000150007)

Zircon U-Pb Ages and Geological Significance of Volcanic Rocks from Maoniushan Formation in the Northern Margin of Qaidam Basin

ZHANG Yaoling1,2(), NI Jinyu3, SHEN Yanxu4, WANG Chaoqun2, GAO Wanli2, HU Daogong2   

  1. 1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
    2. Institute of Geomechanics, Chinese Academy of Geoscience, Beijing 100081, China
    3. Minmetals Exploration and Development Co.Ltd., China Minmetals Corporation,Beijing 100010, China
    4. Cores and Samples Center of Land & Resources, Langfang,Hebei 065201, China
  • Received:2017-07-23 Revised:2017-12-01 Online:2018-04-10 Published:2018-05-07

摘要:

柴北缘牦牛山组磨拉石建造不整合覆盖在前泥盆系之上,记录了该地区早古生代洋盆关闭的时间。对柴北缘牦牛山一带牦牛山组上部火山岩段两个流纹质熔结凝灰岩样品进行锆石U-Pb同位素测定,两个样品的岩浆锆石206Pb/238U年龄加权平均值分别为(396.5±2.4) Ma(n=17,MSWD=3.3)和(395.8±1.2) Ma(n=20,MSWD=1.1),均被解释为火山岩喷发年龄。结合东昆仑造山带牦牛山组测年结果,认为柴达木盆地周缘牦牛山组火山岩形成时代为晚志留世—晚泥盆世,且东昆仑与柴北缘加里东造山作用结束的时间均为早泥盆世之前,而非传统认为的晚泥盆世。

关键词: 牦牛山组, 火山岩, 锆石U-Pb年龄, 泥盆纪, 柴北缘

Abstract:

The molasses of Maoniushan Formation rest unconformably on pre-Devonian strata and record the closure time of the Early Paleozoic ocean in the northern margin of Qaidam Basin. This research determinates zircon U-Pb isotopes from two rhyolite-tuff samples of volcanic rock member of upper Maomiushan Formation of Maoniushan mountain, northern margin of Qaidam Basin. The weighted mean 206Pb/238U ages of magmatic zircons from two samples are (396.5±2.4) Ma(n=17,MSWD=3.3)and (395.8±1.2) Ma(n=20,MSWD=1.1), interpreted as the formation time of the volcanic rocks. Combining past dating results about Maoniushan Formation of East Kunlun orogenic belt, we concluded that the formation time of the Maoniushan Formation around Qaidam Basin should be Late Silurian to Late Devonian, and the Caledonian movement of East Kunlun and northern margin of Qaidam Basin ended before Early Devonian instead of Late Devonian, as traditional thought.

Key words: Maoniushan Formation, volcanic rock, zircon U-Pb age, Devonian, Northern Qaidam Basin

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