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滇东北梅树村期磷矿成矿作用研究进展

熊灿娟 杨瑞东 高军波 陈吉艳 蒋元 李智 彭柔 高川黔 庞雨雨

地质论评2026,Vol.72Issue(1):253-268,16.
地质论评2026,Vol.72Issue(1):253-268,16.DOI:10.16509/j.georeview.2025.05.075

滇东北梅树村期磷矿成矿作用研究进展

Research progress on the ore-forming processes of phosphorite during the Meishucun Period in northeastern Yunnan

熊灿娟 1杨瑞东 2高军波 2陈吉艳 2蒋元 2李智 2彭柔 2高川黔 2庞雨雨2

作者信息

  • 1. 六盘水师范学院,贵州六盘水,553004
  • 2. 贵州大学资源与环境工程学院&喀斯特地质资源与环境教育部重点实验室,贵阳,550025
  • 折叠

摘要

Abstract

Phosphorite,as a vital non-metallic mineral resource,is widely utilized in various fields,including agriculture,industry,and environmental protection.The northeastern Yunnan region,located on the southwestern margin of the Yangtze Craton,is a key area for the distribution of phosphorite resources.Consequently,research on its ore-forming processes holds significant academic and economic value.This review highlights the research progress on the metallogenic geological background,material sources,and ore-forming mechanisms of Cambrian Meishucun period phosphorite deposits in northeastern Yunnan.It is generally accepted that the phosphate deposits in northeastern Yunnan primarily formed in shallow marine carbonate platforms and platform sag basins.However,there remains ongoing debate regarding the specific depositional paleogeography and paleoenvironment.Several viewpoints exist concerning the sources of ore-forming materials,which include terrestrial materials,biogenic phosphorus,seawater,and deep-seated hydrothermal fluids.The main ore-forming mechanisms identified are biogenic phosphogenesis,marine hydrothermal deposition,and upwelling currents.Despite extensive studies on the genesis of phosphorite,no consensus has yet been reached.Controversies persist regarding the metallogenic background,material sources,and ore-forming mechanisms,which have hindered the development of regional metallogenic models.Future research should focus on in situ microstructural analysis combined with various geochemical methods to further explore the genesis mechanisms and paleo-oceanic environment of phosphorite in northeastern Yunnan.This will help establish a comprehensive metallogenic model for the region,contributing to phosphorite resource exploration and development,as well as advancing the study of the metallogenic system of the Yangtze Craton.

关键词

滇东北/磷矿/成矿背景/物质来源/成矿机制

Key words

northeastern Yunnan/phosphorite/metallogenic background/material sources/ore-forming mechanisms

引用本文复制引用

熊灿娟,杨瑞东,高军波,陈吉艳,蒋元,李智,彭柔,高川黔,庞雨雨..滇东北梅树村期磷矿成矿作用研究进展[J].地质论评,2026,72(1):253-268,16.

基金项目

本文为国家重点研发计划(编号:2023YFC2906604)、贵州省毕节地区磷矿调查评价项目、贵州省地质勘查专项资金项目"贵州省威宁县玉龙—岔河地区磷矿调查评价"和贵州省磷矿探矿顶尖专家团队项目(编号:黔科合人才CXTD[2025]013)的成果. Supported by the National Key Research and Development Program of China(No.2023YFC2906604) (编号:2023YFC2906604)

地质论评

0371-5736

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