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华北中部狐偃山杂岩体形成时代研究——来自榍石U-Pb同位素年代学的证据

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何佳佳, 张乔, 靳梦琪, 周俊林, 李玉宏, 陈高潮. 2022. 华北中部狐偃山杂岩体形成时代研究——来自榍石U-Pb同位素年代学的证据. 西北地质, 55(1): 50-63. doi: 10.19751/j.cnki.61-1149/p.2022.01.004
引用本文: 何佳佳, 张乔, 靳梦琪, 周俊林, 李玉宏, 陈高潮. 2022. 华北中部狐偃山杂岩体形成时代研究——来自榍石U-Pb同位素年代学的证据. 西北地质, 55(1): 50-63. doi: 10.19751/j.cnki.61-1149/p.2022.01.004
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HE Jiajia, ZHANG Qiao, JIN Mengqi, ZHOU Junlin, LI Yuhong, CHEN Gaochao. 2022. Chronology Framework of Huyanshan Complex in Central North China Craton: Evidence from U-Pb Dating of Titanite. Northwestern Geology, 55(1): 50-63. doi: 10.19751/j.cnki.61-1149/p.2022.01.004
Citation: HE Jiajia, ZHANG Qiao, JIN Mengqi, ZHOU Junlin, LI Yuhong, CHEN Gaochao. 2022. Chronology Framework of Huyanshan Complex in Central North China Craton: Evidence from U-Pb Dating of Titanite. Northwestern Geology, 55(1): 50-63. doi: 10.19751/j.cnki.61-1149/p.2022.01.004
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华北中部狐偃山杂岩体形成时代研究——来自榍石U-Pb同位素年代学的证据

  • 1. 西安城市发展(集团)有限公司, 陕西 西安 710004;

  • 2. 自然资源部岩浆作用成矿与找矿重点实验室, 中国地质调查局西安地质调查中心, 陕西 西安 710054;

  • 3. 西北地质调查科技创新中心, 陕西 西安 710054

  • 基金项目:

    陕西省科技计划项目“基于U-Th-Pb同位素年代学方法计算华山岩体中氦气资源量”（2021JQ-327），中国地质调查局地质调查项目“关中地区氦气资源调查”（DD20190103），陕西省创新人才推进计划“造山带地层层序恢复：以甘蒙北山造山带南部的石炭—二叠系为例（2021KJXX-74）。

详细信息
    作者简介: 何佳佳(1987-),女,甘肃庆阳人,汉族,工程师,研究方向为地质学。E-mail:hejjia04@163.com。
    通讯作者: 张乔(1992-),男,湖北荆州人,汉族,工程师,研究方向为花岗岩岩石学、岩石成因。E-mail:hotrock2012zq@163.com。

  • 中图分类号: P581

Chronology Framework of Huyanshan Complex in Central North China Craton: Evidence from U-Pb Dating of Titanite

  • 1. Xi'an Urban Development(Group) Co., Ltd., Xi'an 710004, Shaanxi, China;

  • 2. Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MNR, Xi'an Center of China Geological Survey, Xi'an 710054, Shaanxi, China;

  • 3. Northwest Geological Survey Science and Technology Innovation Center, Xi'an, 710054, Shaanxi, China

More Information

    摘要
  • 近年随着定年技术的发展，榍石LA-ICP-MS U-Pb定年法逐渐被学者采用，用来揭示某些特殊岩石类型的形成时代，如碱性岩。华北中部狐偃山碱性杂岩体由多个侵入体组成，岩性主要为二长岩类，岩石中发育大量继承锆石，结晶锆石相对较少，但包含大量岩浆榍石。本次研究即利用榍石LA-ICP-MS U-Pb定年法，对研究相对薄弱的矿泉、狼窝沟2个二长岩体中榍石进行了年代学分析。结果表明这2个二长岩体分别侵位于129 Ma和130 Ma。作为对比，同时对相同2个样品进行了锆石LA-ICP-MS U-Pb定年，2种方法得到的结果在误差范围内一致。结合前人研究资料，狐偃山杂岩体主体二长岩类侵位于早白垩世早期（127~131 Ma），早白垩世晚期（111~114 Ma）有少量正长岩形成，从而构成了狐偃山杂岩体。
    With the development of dating technique, LA-ICP-MS U-Pb dating of titanite has been applied to some special rock types such as alkaline rocks. The Huyanshan alkaline complex was composed of several plutons; the major lithology was monzonite with abundant inherited zircons and magmatic titanites, and little crystallized zircons. This study analyzed chronologically the two monzonites of Kuangquan and Langwogou based on the LA-ICP-MS U-Pb dating of titanite. Results show that the two were emplaced at 129~130Ma. Meanwhile zircon LA-ICP-MS U-Pb dating was conducted on the same two samples as a contrast. The two dating techniques are consistent within the error range. According to previous studies, Monzonites of the main part of Huyanshan complex were emplaced in the early Early Cretaceous (127~131 Ma), while small amount of syenites were formed in the late Early Cretaceous(111~114 Ma),eventually forming the Huyanshan complex.
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收稿日期:  2021-03-11
修回日期:  2021-06-20

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