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滇东南个旧碱性岩的成岩演化与不相容元素富集特征

成飞 晏中海 徐争启 张苏恒 黄迪 冯琪威 宁鹏 张宗博 姚建 张元涛

河北地质大学学报2026,Vol.49Issue(4):22-35,14.
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河北地质大学学报2026,Vol.49Issue(4):22-35,14.DOI:10.13937/j.cnki.hbdzdxxb.2026.04.003

滇东南个旧碱性岩的成岩演化与不相容元素富集特征

Diagenetic Evolution and Enrichment Characteristics of Incompatible Elements of Gejiu Alkaline Rocks in Southeastern Yunnan

成飞 1晏中海 2徐争启 3张苏恒 1黄迪 1冯琪威 1宁鹏 1张宗博 4姚建 2张元涛2

作者信息

  • 1. 成都理工大学地球与行星科学学院,四川 成都 610059
  • 2. 核工业二八○研究所,四川 广汉 618300
  • 3. 成都理工大学地球与行星科学学院,四川 成都 610059||成都理工大学核技术与自动化工程学院,四川 成都 610059||地球勘探与信息技术教育部重点实验室,四川 成都 610059||地学核技术四川省重点实验,四川 成都 610059
  • 4. 成都理工大学核技术与自动化工程学院,四川 成都 610059
  • 折叠

摘要

Abstract

The Gejiu complex rock body develops a complete suite of magmatic rocks ranging from mafic to alkaline.Previous studies have primarily focused on acidic granites related to tin mineralization,with less attention paid to alkaline rocks.Recent discoveries of good enrichment in Th,U,and rare earth elements in alkaline rocks from Changlinggang and Baiyunshan,but their evolution and enrichment processes remain unclear.This paper conducts research on the two rock bodies through field investigations,petrographic and geochemical analyses.The results indicate that the Gejiu alkaline rocks belong to the potassium basalt series,characterized by high Al2O3(13.63%~21.80%),high total alkalis(7.76%~16.72%),low MgO,MnO,and P2O5;they strongly enrich Th(115× 10-6~249 × 10-6),U(26× 10-6~50× 10-6),and REEs(∑ REE=699× 10-6~803 × 10-6),with a right-skewed REE distribution pattern.Zircon U-Pb dating shows they formed during the Late Yanshanian period(82~80 Ma).Comprehensive studies suggest that the rocks exhibit characteristics of a mantle source enriched by subduction fluids,having undergone varying degrees of partial melting and fractional crystallization,with the Changlinggang rock body showing lower degree of melting.The intraplate tectonic environment provided the thermal source for the magmatic crystallization differentiation of the Gejiu alkaline rocks.During crystallization differentiation,the alkaline rocks enriched in Th,U,Nb,and heavy REEs,with highly radioactive enriched biotite veins(Th and U reaching 5 000 × 10-6 and 350 × 10-6,respectively)developed within the rock body,indicating late hydrothermal superimposed enrichment and demonstrating good potential for Th,U,Nb,and REE mineralization.

关键词

岩浆演化/元素富集/碱性岩/个旧杂岩体

Key words

magma evolution/element enrichment/alkaline rock/Gejiu complex

分类

天文与地球科学

引用本文复制引用

成飞,晏中海,徐争启,张苏恒,黄迪,冯琪威,宁鹏,张宗博,姚建,张元涛..滇东南个旧碱性岩的成岩演化与不相容元素富集特征[J].河北地质大学学报,2026,49(4):22-35,14.

基金项目

中国核工业地质局项目(AH2024-0551) (AH2024-0551)

四川省自然科学基金面上项目(2024NSFSC0090) (2024NSFSC0090)

河北地质大学学报

OACHSSCD

1007-6875

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