地学前缘 ›› 2025, Vol. 32 ›› Issue (1): 343-366.DOI: 10.13745/j.esf.sf.2024.4.60

• “印度欧亚大陆碰撞及其远程效应”专栏之十一 • 上一篇    下一篇

中拉萨地体当惹雍措锆石微量元素特征及其对地壳厚度演化的指示

刘晓惠1(), 刘一珉2,*(), 丁林3, 郭晓玉4,5, 黄兴富6, 李蕙琳4,5, 高锐4,5   

  1. 1.中国石油大学(北京) 地球物理学院, 油气资源与工程全国重点实验室, 北京 102249
    2.中国科学院地质与地球物理研究所, 岩石圈演化与环境演变全国重点实验室, 北京 100029
    3.中国科学院青藏高原研究所, 青藏高原地球系统与资源环境重点实验室, 北京 100101
    4.中山大学地球科学与工程学院, 广东 珠海 519082
    5.南方海洋科学与工程广东省实验室(珠海), 广东 珠海 519082
    6.桂林理工大学地球科学学院, 广西 桂林 541004
  • 收稿日期:2024-04-11 修回日期:2024-05-08 出版日期:2025-01-25 发布日期:2025-01-15
  • 通信作者: *刘一珉(1994—),男,博士后,主要从事青藏高原构造地质学研究工作。E-mail: liuymgeo@163.com
  • 作者简介:刘晓惠(1990—),女,讲师,主要从事青藏高原新生代地表隆升及地球深部动力学过程研究工作。E-mail: liuxiaohui@cup.edu.cn
  • 基金资助:
    国家自然科学基金项目(42202237);国家自然科学基金项目(42304105);国家自然科学基金项目(42274120);国家自然科学基金项目(41874102);中国石油大学(北京)科研基金资助项目(2462023YJRC004);科学技术部第二次青藏高原科学考察项目(2019QZKK0701)

Crustal thickness evolution of the Central Lhasa Terrane inferred from trace elements in zircon of Tangra Yumco

LIU Xiaohui1(), LIU Yimin2,*(), DING Lin3, GUO Xiaoyu4,5, HUANG Xingfu6, LI Huilin4,5, GAO Rui4,5   

  1. 1. State Key Laboratory of Petroleum Resources and Prospecting, College of Geophysics, China University of Petroleum (Beijing), Beijing 102249, China
    2. State Key Laboratory of Lithospheric and Environmental Coevolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
    3. State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
    4. School of Earth Sciences and Engineering, Sun Yat-sen University, Zhuhai 519082, China
    5. Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China
    6. College of Earth Sciences, Guilin University of Technology, Guilin 541004, China
  • Received:2024-04-11 Revised:2024-05-08 Online:2025-01-25 Published:2025-01-15

摘要:

拉萨地体位于青藏高原南部,是全球地壳厚度最大的区域之一。然而,拉萨地体地壳增厚的时间和过程仍存在一定争议。锆石的微量元素特征受控于锆石与其他微量元素载体矿物之间的共生关系,即不同矿物的分配系数不同,因此,锆石微量元素可用于定量重建地壳厚度。本研究对来自中拉萨地体当惹雍措地区的岩浆岩和沉积岩中的锆石开展了U-Pb年代学和微量元素地球化学研究。利用锆石的Eu异常对地壳厚度进行定量重建,结果显示,中拉萨地体在侏罗纪至新近纪期间,经历了两次地壳减薄(150~130和85~65 Ma)和两次地壳增厚(130~85和65~15 Ma)事件。在150~130 Ma期间,中拉萨地体地壳减薄主要与班公湖—怒江洋的板片回撤有关。在130~85 Ma期间,由于新特提斯洋向北俯冲和班公湖—怒江洋向南俯冲,中拉萨地体发生了地壳增厚。在85~65 Ma期间,新特提斯洋的板片回撤和弧后拉张导致中拉萨地体再次发生地壳减薄。在65~15 Ma,印度与亚欧板块的碰撞和后续挤压作用,导致中拉萨地体地壳再次加厚。

关键词: 青藏高原, 中拉萨地体, 地壳厚度, 锆石U-Pb年龄, 锆石微量元素

Abstract:

The Lhasa terrane is located in the southern part of the Tibetan Plateau and is one of the regions with the greatest crustal thickness globally. However, the timing and process of crustal thickening in the Lhasa terrane remain debated. Zircon trace element characteristics are controlled by the co-existing relationships between zircon and other trace element carrier minerals, meaning different minerals have varying partition coefficients, thus zircon trace elements can be used to quantitatively reconstruct crustal thickness. This study conducted U-Pb geochronological and trace element geochemical research on zircons from igneous and sedimentary rocks in the Dangra Yongcuo area of the central Lhasa terrane. Using zircon europium anomalies to quantitatively reconstruct crustal thickness, the results reveal that the central Lhasa terrane experienced two crustal thinning events (150-130 Ma and 85-65 Ma) and two crustal thickening events (130-85 Ma and 65-15 Ma) during the Jurassic to Neogene periods. During 150-130 Ma, crustal thinning in the central Lhasa terrane was primarily related to slab retreat of the Bangong-Nujiang Ocean. Between 130-85 Ma, the central Lhasa terrane underwent crustal thickening due to northward subduction of the Neo-Tethys Ocean and southward subduction of the Bangong-Nujiang Ocean. During 85-65 Ma, slab retreat of the Neo-Tethys Ocean and back-arc extension led to another crustal thinning event. From 65-15 Ma, collision and subsequent compression between the Indian and Eurasian plates caused the central Lhasa terrane to thicken again.

Key words: Tibetan Plateau, central Lhasa terrane, crustal thickness, zircon U-Pb age, zircon trace elements

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