| 摘要: |
| 西藏山南隆子县列麦地区始新世花岗岩的成岩时代和背景对喜马拉雅地区同碰撞阶段的构造演化具有重要意义。本文对隆子县列麦乡界归党村的白云母花岗岩开展独居石LA-ICP-MS U-Th-Pb测年，独居石40个测点的208Pb/232Th加权平均年龄为41±0.1Ma（MSWD=1.4），形成于始新世中期。结合区域上的始新世岩浆岩活动和区域变质作用，本文认为在50~45Ma印度下地壳发生中-高压变质和部分熔融；45Ma新特提斯洋洋壳板片断离，软流圈地幔上涌；45~41Ma喜马拉雅发生短暂的拉张环境导致大量的埃达克质岩浆岩侵位和麻粒岩的折返。 |
| 关键词: 始新世 白云母花岗岩 独居石U-Th-Pb年龄 山南地区 喜马拉雅地区 |
| DOI：10.19826/j.cnki.1009-3850.(2020)02-0031-12 |
| 附件 |
| 投稿时间：2020-02-03修订日期：2020-05-04 |
| 基金项目:中国地质调查局项目（西藏山南地区铍锡多金属矿调查评价：DD20190147；冈底斯-喜马拉雅铜矿资源基地调查：DD20160015）；国家自然科学基金项目（41802095） |
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| Monazite U-Th-Pb age of Liemai Eocene granites in the southern Tibet and its geological implications |
| CAO Huawen, LI Guangming, ZHANG Linkui, DONG Lei, GAO Ke, DAI Zuowen |
| (Chengdu Center, China Geological Survey, Chengdu 610081,Sichuan,China) |
| Abstract: |
| The age and tectonic setting of Eocene granites from Liemai in Longzi County, Tibet are of great significance to the tectonic evolution of the Himalayan region in the syncollision stage. In this paper, monazite LA-ICP-MS U-Th-Pb dating has been carried out for muscovite granites in Jieguidang. The weighted average age of 208Pb/232Th is 41 ±0.1 Ma (MSWD=1.4, n=40), which was formed in the Middle Eocene. Combined with the Eocene magmatic rocks and metamorphism in the region, it is considered that the middle high pressure metamorphism and partial melting occurred in the India lower crust at 50-45 Ma. The Neo-Tethys oceanic crust plate separated and the asthenosphere mantle upwelling occurred at 45 Ma. The Himalaya experienced a short-term extension environment, which resulted in a large number of adakitic magmatic rock emplacement and eclogite exhumation at 45-41 Ma. |
| Key words: Eocene muscovite granite monazite U-Th-Pb age Shannan area Himalaya |
