摘要
黔北浣溪铝土矿床为产于石炭系黄龙组灰岩古侵蚀风化面或志留系韩家店组黏土岩、页岩、砂岩等侵蚀间断面之上的一水硬铝石沉积型大型铝土矿床,初步探明铝土矿资源量2000×104余吨。研究表明,浣溪铝土矿床地表矿体质量总体优于深部,地表矿体具有中铁、低硫特征,深部矿体具有中铁、高硫特征。矿石主要化学组分为Al2O3、SiO2、Fe2O3、TiO2及烧失量,占矿石组分的95%~98%,Al2O3与SiO2呈负相关关系;镓、锂是矿床的伴生有益元素。矿床的形成主要受地层岩性、向斜构造、古气候、古沉积环境等因素控制;炎热潮湿的古气候条件和半封闭海湾环境利于成矿。
Huanxi Bauxite Deposit belongs to diasporite sedimentary bauxites deposit which was formed on paleo-erosion weathering surface of carbonate rock of Carboniferous Huanglong formation,or erosion discontinuity surface of clay rock,shale,sandstone of Silurian Hanjiadian formation.The amount of bauxite resources exceeds 20 million tons.Study of the deposit showed that the quality of ores at surface was better than those to depth,i.e.,medium content of iron and low sulfur;ores to depth are of medium Fe content and high sulfur;the ore is mainly composed of Al2O3,SiO2,Fe2O3 and materials of ignition loss,about 95%~98% of the total,and Al2O3 is negatively correlated with SiO2;Gallium,lithium were major beneficial elements.The formation of ore deposit was controlled by lithology,syncline structure,paleoclimate and paleo-sedimentary environment.Bauxite ore occur under condition of semi-closed bay and warm and wet paleoclimate environment.
作者
莫光员
吴启美
顾业平
MO Guangyuan;WU Qimei;GU Yeping(Nuclear Institute of Geological Survey,Guizhou Nonferrous Metals and Nuclear Industry Geological Exploration Bureau,Guiyang 550005,China;Guizhou Normal University,Guiyang 550001,China;Key Laboratory frrinfrrmation System of Mountainous Area and Protection of Ecological Environmentof Guizhou Province,Guizhou Normal University,Guiyang 550001,China;NO.6 General Team,Guizhou Nonferrous Metals and Nuclear Industry Geological Exploration Bureau,Kaili 556000,Guizhou,China)
出处
《地质找矿论丛》
CAS
CSCD
2020年第1期1-7,共7页
Contributions to Geology and Mineral Resources Research
基金
中央地质勘查基金“贵州省道真县浣溪向斜北部铝土矿普查”(编号:2012520001)资助
关键词
浣溪铝土矿
地质特征
控矿因素
黔北地区
Huanxi bauxite deposit
geological characteristic
ore-controlling factors
northern Guizhou province
