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滇东北白龙潭磷矿床地质特征及资源潜力OA

Geological Characteristics and Resource Potential of the Bailongtan Phosphorite Deposit in Northeast Yunnan Providence

中文摘要英文摘要

白龙潭磷矿作为川滇成磷带的重要组成部分,具有矿层厚、品位高、埋藏浅等显著特点.本文基于矿区详细勘查资料,系统总结了区域地质特征、矿体展布规律、矿石及风化矿特征,并对深部及边部资源潜力进行了评价.研究结果表明,矿石自然类型以致密块状磷块岩、白云质磷块岩、硅质磷块岩和泥质磷块岩为主,工业类型主要为硅质及硅酸盐型,属于典型的浅海相沉积磷块岩矿床.风化带分布范围有限,主要集中于矿区北部的干龙包包及白龙潭一带.上矿层K4浅部以风化-半风化矿石为主,P2O5品位普遍高于28%,深部原生矿品位稳定在24%左右,品位变化范围为16.39%~34.34%,变化系数为15.92%.矿体厚6~8m,变化系数为38.28%;下矿层K2主要为原生矿,厚0.75~5.87m,平均2.65m,向南深部趋于稳定在4m左右,变化系数为49.97%,品位变化范围为15.01%~26.05%,变化系数为13.53%.总体来看,上矿层K4和下矿层K2南深部厚度与品位均较为稳定.综合分析,矿区南部找矿潜力较大,具备大型磷矿床资源前景.

The Baitanlong phosphate deposit,as an important part of the Sichuan-Yunnan phosphorite belt,exhibits significant characteristics such as thick ore layers,high grade,and shallow burial.Based on detailed exploration data of the mining area,this paper systematically summarizes regional geological characteristics,orebody distribution patterns,characteristics of primary ore and weathered ore,and evaluates resource potential in the deep and marginal areas.The results show that the natural ore types are mainly dense massive phosphate rock,dolomitic phosphate rock,siliceous phosphate rock and argillaceous phosphate rock.The industrial ore type is mainly siliceous-silicate type,belonging to a typical shallow marine sedimentary phosphate deposit.The weathered zone is limited in distribution,mainly concentrated in Ganlongbaobao and Baitanlong in the northern mining area.The shallow part of upper ore bed K4 is dominated by weathered and semi-weathered ore with P2O5 grade generally higher than 28%,while the deep primary ore grade remains stable at around 24%.The orebody thickness ranges from 6 to 8 m with a variation coefficient of 38.28%,and the grade varies from 16.39%to 34.34%with a variation coefficient of 15.92%.The lower ore bed K2 is mainly primary ore with a thickness of 0.75~5.87 m(average 2.65 m),tending to stabilize at about 4 m in the southern deep area with a thickness variation coefficient of 49.97%,and its grade ranges from 15.01%to 26.05%with a variation coefficient of 13.53%.Overall,both thickness and grade of K4 and K2 orebodies are stable in the southern deep mining area.Comprehensive analysis indicates that the southern part of the mining area has significant prospecting potential and prospects for a large-scale phosphate deposit.

张成信;高磊;伍光锋;金松;杨立朋;于汪;袁绍金;高军波;王畅;王艳超

中化地质矿山总局地质研究院,北京 100101||贵州大学资源与环境工程学院,贵州贵阳 550025中国地质科学院矿产资源研究所,北京 100037中化地质矿山总局地质研究院,北京 100101中化地质矿山总局地质研究院,北京 100101中化地质矿山总局地质研究院,北京 100101中化地质矿山总局地质研究院,北京 100101昆明市中航磷化工有限公司,云南 昆明 654199贵州大学资源与环境工程学院,贵州贵阳 550025中化地质矿山总局地质研究院,北京 100101中化地质矿山总局地质研究院,北京 100101

天文与地球科学

梅树村组白龙潭磷矿矿体特征风化矿资源潜力滇东北

Meishucun FormationBailongtan phosphate depositOre body characteristicsWeathered oreResource potentialNortheast Yunnan Province

《化工矿产地质》 2026 (2)

97-104,8

深地国家科技重大专项(编号:2024ZD1002004)、国家重点研发计划项目(编号:2023YFC2906604)、云南省昆明市东川区白龙潭磷矿生产勘探项目(编号:2022-J2353)、自然资源部"战略化工矿产成矿理论及找矿技术创新团队"(编号:ZRC-TD2023056)

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