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四川雷波县巴姑磷矿矿床地质特征及成因探讨

马殿哲 刘坤 龙有根

中国非金属矿工业导刊Issue(5):49-54,6.
中国非金属矿工业导刊Issue(5):49-54,6.

四川雷波县巴姑磷矿矿床地质特征及成因探讨

Geological Characteristics and Genesis of Bagu Phosphate Deposit in Leibo County,Sichuan Province

马殿哲 1刘坤 1龙有根2

作者信息

  • 1. 山东省地矿工程集团有限公司,山东 济南 250000
  • 2. 四川省地球物理调查研究所,四川 成都 610072
  • 折叠

摘要

Abstract

The Bagu Phosphate Mine is located in the southwestern part of Leibo County,Sichuan Province,and is a shallow marine layered carbonate phosphate rock deposit.The phosphate ore is hosted in the middle section of the Maidiping Formation.The ore bodies include No.I and No.II,with the grade of No.II ore body(average grade of 24.62%)being higher than that of No.I ore body(average grade of 21.33%).The ore types are mainly dense massive phosphate rock,striped and banded phosphate rock,and porous phosphate rock.The structures are mainly sandy clastic,followed by gravelly sandy clastic,oolitic,and micritic structures.The ore minerals are mainly colloidal apatite and minor crystalline apatite.Based on a comprehensive analysis of previous research results,it is concluded that the source of the mineralizing material of the Bagu Phosphate Mine is mainly seawater and is closely related to biological activity.The synsedimentary basin formed at the depression site is a favorable structure for mineralization.The sedimentary environment directly affects the physical enrichment of phosphate ore.The high-energy subtidal facies during the regression-transgression transition period is a favorable facies belt for phosphate deposition and is a key area for future exploration and development.

关键词

磷矿/麦地坪组/同沉积盆地/高能潮下滩相

Key words

phosphate rock/Maidiping Formation/synsedimentary basin/high-energy subtidal beach facies

分类

天文与地球科学

引用本文复制引用

马殿哲,刘坤,龙有根..四川雷波县巴姑磷矿矿床地质特征及成因探讨[J].中国非金属矿工业导刊,2025,(5):49-54,6.

中国非金属矿工业导刊

1007-9386

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