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云南峨山塔甸地区中元古界黑山头组石英岩矿地质特征

李维科 刘军平 晏海宝 胡绍斌 何世军 赵江泰 赵云江 魏思礼

地球学报2024,Vol.45Issue(4):493-501,9.
地球学报2024,Vol.45Issue(4):493-501,9.DOI:10.3975/cagsb.2024.042801

云南峨山塔甸地区中元古界黑山头组石英岩矿地质特征

Geological Characteristics of Quartzite Deposits of Mesoproterozoic Heishantou Formation in Tadian Area,Eshan,Yunnan Province

李维科 1刘军平 2晏海宝 3胡绍斌 1何世军 4赵江泰 3赵云江 3魏思礼3

作者信息

  • 1. 云南省地质调查院,云南昆明 650216||自然资源部三江成矿作用及资源勘查利用重点实验室,云南昆明 650051
  • 2. 云南省地质调查院,云南昆明 650216||自然资源部三江成矿作用及资源勘查利用重点实验室,云南昆明 650051||中国地质大学(北京)地球科学与资源学院,北京 100083
  • 3. 云南省地质调查院,云南昆明 650216
  • 4. 中国冶金地质总局第二地质勘查院,福建福州 350108
  • 折叠

摘要

Abstract

Based on the 1:50 000 regional geological survey,typical profile and notch sampling,the Mesoproterozoic Heishantou Formation in the Tadian area of Eshan,Yunnan Province,has identified several layers of quartzite deposits with a thickness of approximately 104-227 m.The ore-bearing lithology is gray-white,ivory-thick layered quartzite,with aphanitic-granular metamorphic structure,mainly composed of quartzite(>95%).The analysis shows that the sample contains 95.15%-99.41%SiO2,0.21%-2.61%Al2O3,0.008%-0.047%CaO,0.088%-0.47%TFe2O3,0.009%-0.56%K2O,and 0.010%-0.13%MgO.The content of TiO2 is 0.011%-0.06%,which partially meets the industrial index requirements of siliceous raw materials such as glass and crystalline silicon.Heishantou Formation quartzite is an ore body with multi-layered occurrence and large monomer thickness,with a stable horizon and long extension.It is a set of coastal sedimentary metamorphic quartzite deposits with great potential value and economic benefits,and is expected to form a large-scale quartzite raw material-producing area in the future.

关键词

峨山地区/中元古界/黑山头组/石英岩矿/沉积变质型/找矿潜力

Key words

Eshan area/Mesoproterozoic/Heishantou Formation/quartzite ore/sedimentary metamorphic type/prospecting potential

分类

天文与地球科学

引用本文复制引用

李维科,刘军平,晏海宝,胡绍斌,何世军,赵江泰,赵云江,魏思礼..云南峨山塔甸地区中元古界黑山头组石英岩矿地质特征[J].地球学报,2024,45(4):493-501,9.

基金项目

本文由云南省自然资源厅基金项目"云南 1:5 万大庄幅、法裱幅、底土幅、甸中幅区域地质调查"(编号:D202207)和云南省科技计划项目(编号:202305AD160031 (编号:D202207)

202401AT070012)联合资助. This study was supported by Department of Nat-ural Resources of Yunnan Province(No.D202207),and Science and Technology Plan Project of Yunnan Province(Nos.202305AD160031 and 202401AT070012). (No.D202207)

地球学报

OA北大核心CSTPCD

1006-3021

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