中国非金属矿工业导刊Issue(2)：12-15,4.
豫西张窑院耐火粘土矿床地质特征研究
Study on Geological Characteristics of Zhangyaoyuan Refractory Clay Deposit in Western Henan
摘要
Abstract
The refractory clay deposit is gently tilted and stratified in the Carboniferous Benxi Formation,and the orebodies are mainly composed of high-alumina clays and hard clays.Through the ore chemical analysis,microscopic characteristics and XRD analysis,the main components are monohydrate diaspore and kaolinite.The endothermic peak temperature of the ore is about 535℃ and the exothermic peak temperature is about 980℃,which is obtained by differential thermal analysis curves.It is believed that the ore-beating strata of Benxi Formation strata inherited the paleo-continental weathering crust formed since Middle Ordovician,bottomup chip by weathering crust depression crater where land filling to the upper epicontinental coastal swamp facies,formed the known as the Fe-Al layer of ore-bearing rock series,different clay layer formed by all kinds of clay minerals,the occurrence and distribution characteristics of the ore-bearing strata are mainly controlled by the ancient karst landform and weathering crust topography of the north-south tectonic fissures.关键词
耐火粘土/XRD/差热分析/古陆风化壳Key words
refractory clay/XRD/differential thermal analysis/the paleo-continental weathering crust分类
天文与地球科学引用本文复制引用
梁新辉,冯绍平,高晓,王小涛,张争辉,张怡静..豫西张窑院耐火粘土矿床地质特征研究[J].中国非金属矿工业导刊,2017,(2):12-15,4.基金项目
河南省“两权价款”地质科研项目(2015-258-03). （2015-258-03）
