武夷山中段建宁地区淡色花岗岩形成时代、地球化学特征及地质意义

卢运可, 辛宇佳, 李建华, 王金铭. 2024. 武夷山中段建宁地区淡色花岗岩形成时代、地球化学特征及地质意义[J]. 地球学报, 45(6): 926-940. doi: 10.3975/cagsb.2023.120501
引用本文: 卢运可, 辛宇佳, 李建华, 王金铭. 2024. 武夷山中段建宁地区淡色花岗岩形成时代、地球化学特征及地质意义[J]. 地球学报, 45(6): 926-940. doi: 10.3975/cagsb.2023.120501
LU Yunke, XIN Yujia, LI Jianhua, WANG Jinming. 2024. Geochronological and Geochemical Constraints of Leucogranites in Jianning Area, Central Wuyishan, and Their Geological Implications. Acta Geoscientica Sinica, 45(6): 926-940. doi: 10.3975/cagsb.2023.120501
Citation: LU Yunke, XIN Yujia, LI Jianhua, WANG Jinming. 2024. Geochronological and Geochemical Constraints of Leucogranites in Jianning Area, Central Wuyishan, and Their Geological Implications. Acta Geoscientica Sinica, 45(6): 926-940. doi: 10.3975/cagsb.2023.120501

武夷山中段建宁地区淡色花岗岩形成时代、地球化学特征及地质意义

  • 基金项目:

    本文由国家自然科学基金项目(编号: 42102274)和自然资源部古地磁与古构造重建重点实验室开放课题(编号: KLPTR-09)联合资助

详细信息
    作者简介: 卢运可, 男, 1997 年生。硕士研究生。地质工程专业。E-mail: luyunke2021@163.com
    通讯作者: 辛宇佳, 男, 1988 年生。博士, 副研究员。主要从事岩石地球化学研究。E-mail: xinyujiacags@cags.ac.cn
  • 中图分类号: P588.121

Geochronological and Geochemical Constraints of Leucogranites in Jianning Area, Central Wuyishan, and Their Geological Implications

More Information
    Corresponding author: XIN Yujia
  • 淡色花岗岩是了解造山过程中地壳物质部分熔融行为的重要岩石探针, 对于揭示造山演化过程中变质和岩浆作用之间的联系具有十分重要的意义。本文对武夷山中段建宁地区淡色花岗岩开展了系统的岩石学、锆石 U-Pb 年代学及地球化学研究。结果表明, 建宁淡色花岗岩形成于~440 Ma, 并记录了晚期410~405 Ma 深熔事件。淡色花岗岩属强过铝质岩石, 且富含800~700 Ma 年龄继承锆石, 表明其源岩为新元古代麻源群变质沉积岩。建宁淡色花岗岩具高SiO2、K2O, 贫MgO、FeOt、CaO、Na2O, 富集LREE 和LILEs, 亏损HREE 和HFSEs, 高Rb/Sr 比值等特征, 暗示其源岩可能发生了黑云母参与的含水或脱水熔融反应。综合本文结果和华南早古生代沉积、变质、岩浆等多方面地质记录可知, 建宁地区淡色花岗岩形成于同造山地壳加厚背景下, 而晚期410~405 Ma 的深熔事件可能与后造山伸展减薄有关。
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出版历程
收稿日期:  2023-11-16
修回日期:  2023-12-01

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