地学前缘 ›› 2022, Vol. 29 ›› Issue (2): 218-233.DOI: 10.13745/j.esf.sf.2021.7.11

• 洋板块地质与造山带地质 • 上一篇    下一篇

江南造山带西段桂北四堡地区830 Ma辉长岩锆石SIMS U-Pb年代学和岩石地球化学特征及其岩石成因研究

寇彩化1(), 刘燕学1,*(), 李江2, 李廷栋1, 丁孝忠1, 刘勇1, 靳胜凯3   

  1. 1.中国地质科学院 地质研究所, 北京 100037
    2.广西壮族自治区地质调查院, 广西 南宁 530023
    3.中国地质大学(北京), 北京 100083
  • 收稿日期:2021-04-30 修回日期:2021-06-02 出版日期:2022-03-25 发布日期:2022-03-31
  • 通讯作者: 刘燕学
  • 作者简介:寇彩化(1985—),女,副研究员,主要从事岩石地球化学研究。E-mail: caihuakou@163.com
  • 基金资助:
    中国地质调查局项目(1212011120117);中国地质调查局项目(1212011120115);国家自然科学基金项目(41972069)

Geochronology and geochemistry of 830 Ma gabbro in the western segment of the Jiangnan Orogen and constraint on its petrogenesis

KOU Caihua1(), LIU Yanxue1,*(), LI Jiang2, LI Tingdong1, DING Xiaozhong1, LIU Yong1, JIN Shengkai3   

  1. 1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
    2. Guangxi Zhuang Autonomous Region Geological Survey Institute, Nanning 530023, China
    3. China University of Geosciences (Beijing), Beijing 100083, China
  • Received:2021-04-30 Revised:2021-06-02 Online:2022-03-25 Published:2022-03-31
  • Contact: LIU Yanxue

摘要:

本次研究对象为江南造山带西段桂北四堡地区新元古代辉长岩,主要由斜长石和单斜辉石组成,含有少量的橄榄石和钛铁氧化物,表明在岩浆演化过程中发生了斜长石和单斜辉石以及少量橄榄石的分离结晶作用。辉长岩锆石SIMS U-Pb谐和年龄为(830±7)Ma,指示其侵位年龄约为830 Ma。全岩具有低SiO2含量(48.46%~53.99%)、高MgO含量(9.27%~25.22%)、Mg#值较高(62~79)的特征。辉长岩为钙碱性系列岩石,其稀土元素球粒陨石标准化和微量元素原始地幔标准化与典型的弧岩浆相似,具有相对富集轻稀土元素((La/Yb)N=2.2~3.7,(La/Sm)N=2.5~2.9)和大离子亲石元素,明显的高场强元素(Nb、Ta和Ti)亏损的特征,还具有较高的Th/Nb比值(0.7~0.8)和低Nb/La比值(0.4~0.6)。辉长岩具有负的εNd(t)值(-6.3~-3.0)和正的εHf(t)值(8.0~12.1),指示其源区为亏损地幔,但有富集组分加入。结合区域地质特征,推测辉长岩形成于活动大陆边缘俯冲构造背景,起源于受沉积物流体交代了的楔地幔。

关键词: 江南造山带西段, 新元古代基性岩, 锆石SIMS U-Pb年龄, 岩石成因, 构造背景

Abstract:

We report gabbro discovered in the western segment of the Jiangnan Orogen Belt, Sibao area, northern Guangxi Province. The gabbro contains mostly plagioclase and clinopyroxene and a small amount of olivine and Fe-Ti oxide minerals, indicating likely fractionation of plagioclase, clinopyroxene and some olivine within the magma chamber. The gabbro specimen has a zircon SIMS U-Pb age of (830±7) Ma, suggesting gabbro emplacement at ~830 Ma. The bulk-rock is characterized by relatively low SiO2 (48.46%-53.99%) and high MgO (9.27%-25.22%) contents with Mg# of 62-79. It belongs to typical calc-alkalic arc rock, characterized by enrichments of light rare earth elements and large-ion lithophile elements relative to heavy rare earth elements ((La/Yb)N=2.2-3.7, (La/Sm)N=2.5-2.9), significantly negative Nb, Ta and Ti anomalies, and relatively high Th/Nb (0.7-0.8) and low Nb/La (0.4-0.6) ratios. The gabbro specimen has negative εNd(t) (-6.3--3.0) and positive εHf(t) (8.0-12.1), indicating it is sourced from depleted mantle with the addition of enriched components. In combination with the regional geology, we infer the gabbro is derived from depleted mantle wedge metasomatized by sediment-derived fluids and formed in the active continental margin in a subduction setting.

Key words: western Jiangnan Orogen, Neoproterozoic mafic intrusion, Zircon SIMS U-Pb dating, petrogenesis, tectonic setting

中图分类号: