我国凹凸棒石黏土矿床成因类型及时空分布规律OA
Genesis Types and Spatiotemporal Distribution Patterns of Attapulgite Clay Deposits in China
凹凸棒石黏土具有独特的晶体结构、强吸附性、催化性等优异性能,在新能源、新材料、节能环保、生物医药等新兴产业中具有重要作用.根据成矿地质作用,本文将凹凸棒石黏土成因类型划分为陆相火山岩型、蒸发沉积型、化学沉积型和风化型 4 种.矿床一般产于构造稳定地区的干旱或半干旱的内陆碱湖、盐湖盆地,碱性玄武岩盆地、浅海碳酸盐岩台地等.主要形成于新生代,空间上主要分布于Ⅱ-68 苏北(断陷)和Ⅲ-18 阿拉善(隆起)成矿带.我国苏皖交界处的明光、来安、盱眙以及六合等县区和甘肃会宁县、临泽地区是我国凹凸棒石最为重要分布区域.
Attapulgite clay possesses excellent properties such as a unique crystal structure,strong adsorption capacity,and catalytic activity,and plays an important role in emerging industries including new energy,advanced materials,energy conservation and environmental protection,and biomedicine.Based on ore-forming geological processes,this paper classifies the genetic types of attapulgite clay into four categories:continental volcanic rock type,evaporative sedimentary type,chemical sedimentary type,and weathering type.Orebodies are generally hosted in arid or semi-arid inland alkali lakes,salt lake basins,alkaline basalt basins,and shallow marine carbonate platforms in tectonically stable areas.They were mainly formed in the Cenozoic Era and are spatially distributed primarily in the Ⅱ-68 Northern Jiangsu(Fault Basin)Metallogenic Belt and the Ⅲ-18 Alxa(Uplift)Metallogenic Belt.The most important distribution areas of attapulgite in China are Mingguang,Lai'an,Xuyi,and Liuhe counties at the junction of Jiangsu and Anhui provinces,as well as Huining County and Linze area in Baiyin city,Gansu province.
颜玲亚;于海军;蔡一鸣;王海成;欧阳友和;李旭
中国建筑材料工业地质勘查中心山东总队,山东 济南 250100中国建筑材料工业地质勘查中心,北京 100035中国建筑材料工业地质勘查中心,北京 100035中国建筑材料工业地质勘查中心山东总队,山东 济南 250100中国建筑材料工业地质勘查中心山东总队,山东 济南 250100中国建筑材料工业地质勘查中心山东总队,山东 济南 250100
天文与地球科学
凹凸棒石黏土典型矿床成因类型时空分布
attapulgite claytypical ore depositsgenetic typesspatiotemporal distribution
《中国非金属矿工业导刊》 2026 (1)
1-6,6
中国地质调查局地质调查项目"中国矿产地质志"资助(编号:DD20221695,DD20190379)中国建筑材料工业地质勘查中心"国外重点非金属矿产信息平台建设项目"资助(编号:建地科[2024]03号).
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