欢迎访问现代地质!

现代地质 ›› 2025, Vol. 39 ›› Issue (03): 715-727.DOI: 10.19657/j.geoscience.1000-8527.2025.022

• 机器学习与矿物学应用 • 上一篇    下一篇

海南岛西部抱板杂岩中伟晶岩矿物学与全岩地球化学特征及成因意义

恽虎1,2,3(), 官军1,4, 王成4,*(), 林世莉1,4, 费光春1,3   

  1. 1.海南省海洋地质资源与环境重点实验室,海南 海口 570206
    2.安徽省核工业勘查技术总院,安徽 芜湖 241000
    3.成都理工大学 地球与行星科学学院,四川 成都 610059
    4.海南省地质调查院,海南 海口 570206
  • 出版日期:2025-06-10 发布日期:2025-07-03
  • 通信作者: *王成,男,高级工程师,1983年出生,主要从事矿产普查与勘探工作。Email:104719830@qq.com
  • 作者简介:恽虎,男,硕士研究生,1998年出生,主要从事矿产普查与勘探工作。Email:869241522@qq.com
  • 基金资助:
    海南省海洋地质资源与环境重点实验室开放课题(22-HNHYDZZYHJKF021)

Mineralogy and Whole Rock Geochemical Characteristics and Genetic Implications of Pegmatites in the Baoban Complex, Western Hainan Island

YUN Hu1,2,3(), GUAN Jun1,4, WANG Cheng4,*(), LIN Shili1,4, FEI Guangchun1,3   

  1. 1. Hainan Key Laboratory of Marine Geological Resources and Environment, Haikou, Hainan 570206, China
    2. Anhui Nuclear Exploration Technology Central Institute, Wuhu, Anhui 241000, China
    3. College of Earth and Planetary Science, Chengdu University of Technology, Chengdu, Sichuan 610059, China
    4. Hainan Institute of Geological Survey, Haikou, Hainan 570206, China
  • Published:2025-06-10 Online:2025-07-03

摘要:

海南岛西部抱板杂岩中广泛发育伟晶岩,但伟晶岩地球化学研究尚未开展,伟晶岩类型、成因及其稀有金属成矿潜力尚不清楚。本文在野外调查和岩石薄片显微观察的基础上,对抱板杂岩中伟晶岩样品开展全岩、单矿物(云母、长石)的主量元素、微量元素和稀土元素分析和长石X射线粉晶衍射分析。划分伟晶岩类型,探讨伟晶岩成因,分析伟晶岩成矿潜力。抱板杂岩中伟晶岩属于白云母钠长石型伟晶岩,具有高硅铝,低钙镁及过铝质等特征;微量元素总体相对富集大离子亲石元素,相对亏损高场强元素;轻稀土元素相对富集,重稀土元素相对亏损。电子探针分析表明伟晶岩中云母主要为白云母,长石主要为钠长石、次为更长石、微斜长石。伟晶岩演化程度低,类型上属于白云母-稀有金属伟晶岩-REE亚类中的褐帘石-独居石子类。伟晶岩全岩和单矿物中的稀有金属含量低,微斜长石晶胞体积小于富铷伟晶岩,不具备形成稀有金属伟晶岩的潜力。

关键词: 花岗伟晶岩, 地球化学, 抱板杂岩, 海南岛

Abstract:

In western Hainan Island, pegmatites were widely distributed in the Baoban Complex. The geochemical research of pegmatites has not been carried out, and the types, genesis and rare metal metallogenic potential are still unclear. Based on field geological characteristics and microscopic observations, major elements, trace elements and rare earth elements of whole rock and single minerals (mica,feldspar) and feldspar X-ray powder diffraction were carried out on pegmatites in the Baoban complex. The type of pegmatites is classified, the metallogenic potential of pegmatites is analyzed, and its genetic relationship between pegmatites and adjacent granites are discussed. The pegmatites belong to the muscovite albite pegmatite, which have high silicon and aluminum content, low calcium and magnesium content and peraluminous. Trace elements are generally enriched in large ion lithophile elements, and depleted in high field strength elements. Light rare earth elements are relatively enriched, while heavy rare earth elements are relatively depleted. Electron Probe Micro-Analysis shows that the mica in the pegmatites is mainly muscovite, and the feldspar is mainly albite, the second oligoclase and microcline. The pegmatites have a low degree of evolution. The pegmatites are classified as the allanite-monazite type of muscovite-rare-element-REE(REL-REE)subclass. The content of rare metals in pegmatites is low, and the cell volume of microcline is smaller than that of rubidium-rich pegmatite. The pegmatites do not have rare metal mineralization potential.

Key words: granite pegmatite, geochemistry, Baoban Complex, Hainan Island

中图分类号: