摘要
粘土矿物是地表带分布最广的矿物,粘土矿物的形成方式有3种:与风化作用有关;热液和温泉水作用于围岩,可以形成粘土矿物的蚀变富集带;由沉积作用、成岩作用生成粘土矿物。对其粘土矿物的成因进行了分析归纳。
Clay mineral is the most widely distributed mineral on surface band. The formation of clay mineral have three ways. Firstly it is related to weathering;Second-ly it is related to alteration. Lastly sedimentation and diagenesis generates clay mineral. This article is analysed and concluded on the formation of clay mineral.
出处
《河北联合大学学报（自然科学版）》
CAS
2013年第1期68-72,共5页
Journal of Hebei Polytechnic University:Social Science Edition
关键词
粘土矿物
风化作用
蚀变
沉积作用
成岩作用
clay mineral
weathering
alteration
sedimentation and diagenesis
