吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (1): 169-184.doi: 10.13278/j.cnki.jjuese.20190229

• 地质与资源 • 上一篇    

滇西兰坪皂角场新生代富碱斑岩体锆石U-Pb年代学及岩石地球化学特征

李守奎1,2, 张世涛1, 赵庆红2, 黎明2   

  1. 1. 昆明理工大学国土资源工程学院, 昆明 650032;
    2. 云南省地质矿产勘查院, 昆明 650051
  • 收稿日期:2019-10-31 发布日期:2021-02-02
  • 通讯作者: 张世涛(1965-),男,教授,博士生导师,主要从事区域地质与成矿作用方面的研究,E-mail:zhangshitao9918@sina.com E-mail:zhangshitao9918@sina.com
  • 作者简介:李守奎(1986-),男,博士研究生,主要从事区域地质、矿产地质方面的研究,E-mail:289749859@qq.com
  • 基金资助:
    中国地质调查局项目（DD20160016）

Zircon U-Pb Chronology and Petrogeochemistry of Cenozoic Alkali-Rich Porphyry in Zaojiaochang, Lanping, Western Yunnan

Li Shoukui1,2, Zhang Shitao1, Zhao Qinghong2, Li Ming2   

  1. 1. Faculty of Land Resource Engineering, Kunming University of Science and Technology, Kunming 650032, China;
    2. Yunnan Institute of Geology & Mineral Resources Exploration, Kunming 650051, China
  • Received:2019-10-31 Published:2021-02-02
  • Supported by:
    Supported by the Project of China Geological Survey (DD20160016)

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摘要： 滇西兰坪盆地因其可观的资源规模和巨大的找矿潜力而倍受地质学界关注，但盆地内部仅有的3处新生代侵入岩之一的皂角场岩体缺少研究，这在一定程度上既影响了对盆地演化和成矿机制的全面认识，也影响了滇西富碱斑岩带研究的完整性。本文对皂角场岩体开展了岩相学、锆石U-Pb年代学、元素地球化学研究。结果显示：皂角场岩体由二长花岗岩（中央相）和花岗闪长斑岩（边缘相）组成；LA-ICP-MS锆石U-Pb定年结果表明岩体侵位时代约为34 Ma；岩石样品具有高硅（w（SiO2）=71.49%~73.17%）、过铝质（A/CNK=1.12~1.32）、富碱（w（K2O+Na2O）=7.83%~9.10%）特征，属高钾钙碱性系列；富集Rb、Ba、Th、U、K和Hf等大离子亲石元素，亏损Ta、Nb、Ti、P等高场强元素，轻稀土元素富集，Eu负异常微弱，具有特殊的Nb/Ta、Th/U值，表明岩浆来源深，母岩浆来源于交代岩石圈地幔源，并受到了壳源物质的混染。综合研究表明：青藏高原晚碰撞期（40~26 Ma）陆内俯冲诱发了地幔物质侧向流动和深部软流圈上涌，形成了富碱斑岩带；而皂角场岩体形成于始新世晚期兰坪盆地盆山转换阶段的陆内造山挤压构造环境，盆地中央具有岩石圈断裂属性的兰坪—思茅中轴大断裂在该时期活动达到顶峰，引发岩浆沿断裂上侵，并在近地表脆性条件下就位形成超浅成富碱斑岩体。

关键词: 皂角场岩体, 富碱斑岩, 兰坪盆地, 锆石U-Pb定年, 岩石地球化学, 岩石成因

Abstract: Lanping basin in western Yunnan has attracted wide attention in geological circles because of its large scale resources and great prospecting potential, however,as one of the only three Cenozoic intrusions in the basin, the Zaojiaochang intrusion is rarely reported. To some extent, this not only affects the overall understanding of the basin evolution and metallogenic mechanism, but also is incomplete for the study of alkali-rich porphyry belt in western Yunnan. A study on petrography, zircon U-Pb chronology and elemental geochemistry, shows that the Zaojiaochang intrusion is composed of monzogranite (central facies) and granodiorite porphyry (marginal facies). The LA-ICP-MS zircon U-Pb dating shows that the emplacement age of the Zaojiaochang intrusion is about 34 Ma. The intrusion belongs to high-K calcium-alkali series, with high silicon (w(SiO2)=71.49%-73.17%), peraluminous (A/CNK=1.12-1.32), and high total alkali (w(K2O+Na2O)=7.83%-9.10%). It is rich in LILEs (Rb, Ba, Th, U, K, Hf) and LREEs, relatively depleted of HFSEs (Ta, Nb, Ti and P), with no or weak negative Eu anomalies and special Nb/Ta and Th/U values. Based on the above mentioned data,it is suggested that the magma of the Zaojiaochang intrusion came from deep source, and the parent magmas originated from a metasomatic lithospheric mantle source, and mixed up with crust-source materials later. The comprehensive study shows that the intracontinental subduction of the Tibetan Plateau during the late collision period (40-26 Ma) induced the lateral flow of mantle material,the upwelling of deep asthenosphere, and the forming of the alkali-rich porphyry belt. The Zaojiaochang intrusion was formed in the Late Eocene Lanping basin transformation stage and the mountain intracontinental orogenic extrusion tectonic environment. In the center of the basin, the Lanping-Simao central axis fault with lithospheric fault property reached its peak in this period, and the magma rose along the fault and formed the super hypabyssal alkaline-rich porphyry under a brittle condition near the surface.

Key words: Zaojiaochang instrution, alkaline-rich porphyries, Lanping basin, zircon U-Pb dating, lithogeochemistry, petrogenesis

中图分类号: 

  • P588.1
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