粘土矿物的成因初步研究  

The Preliminary Research on the Cause of the Clay Minerals

作　　者：徐叶净[1] 左文哲[1] 

机构地区：[1]河北联合大学,河北唐山063009

出　　处：《河北联合大学学报（自然科学版）》2013年第1期68-72,共5页Journal of Hebei Polytechnic University:Social Science Edition

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.

关 键 词：粘土矿物 风化作用 蚀变 沉积作用 成岩作用 

分 类 号：P578.94[天文地球—矿物学]