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宁武──静乐盆地中部煤系高岭岩的特征及成因
引用本文:景贵飞,王式光.宁武──静乐盆地中部煤系高岭岩的特征及成因[J].煤田地质与勘探,1995,23(1):1-8.
作者姓名:景贵飞  王式光
作者单位:北京大学地质学系 100871
摘    要:通过对宁武-静乐盆地中部高岭岩的组成、产状及稀土和微量元素地球化学特征的研究,发现了K+Na+Ca、TiO2、Nb、Zr等与高岭石含量间的正相关关系,讨论了细粒沉积物于沼泽中可能的沉降与扩散机制,认为研究区高岭岩为阴山古陆酸性陆源岩风化产物经搬运沉积后,又在沼泽环境中经淋滤进-步富集而成。 

关 键 词:高岭土    沉积矿床    沼泽环境    沼泽沉积作用    宁武-静乐盆地
收稿时间:1994-03-11

GEOCHEMISTRY AND ORIGIN OF TONSTEINS IN MIDDLE OF NINGWU-JINGLE BASIN,SHANXI PROVINCE
Jing Guifei, Wang Shiguang.GEOCHEMISTRY AND ORIGIN OF TONSTEINS IN MIDDLE OF NINGWU-JINGLE BASIN,SHANXI PROVINCE[J].Coal Geology & Exploration,1995,23(1):1-8.
Authors:Jing Guifei  Wang Shiguang
Institution:Department of Geology, Peking University
Abstract:n the studies of the occurences, compositions and geochemical characteristics of the tonsteins in middle of Ningwu--Jingle Basin,We found the positive correlations between elements of Nb,Zr,(K + Na + Ca). and TiO2 and the contents of kaolinite, discussed the probable sedimentary and spreading mechanisms of fine--grained sediments in swamp,as well as proposing the view that the local tonsteins were formed by leaching and concentration of the weathering products of medi--acid igneous rocks of Yinshan palaeoland which were transported and sedimented in swamp.
Keywords:Kaolin  sedimentary deposits  marsh environment  Paludal sedimentation  Ningwu-Jingle basin    
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