斜坡风化壳元素迁移规律分析  

Analysis of shift regularity of elements in slope's weathering shell

作　　者：刘泉[1] 王志强[1] 

机构地区：[1]昆明理工大学土木系,云南昆明650224

出　　处：《矿业工程》2009年第5期15-17,共3页Mining Engineering

摘　　要：阐述了各种元素随着岩石中造岩矿物的风化、次生矿物生成,发生了迁移。在浅表生带中,元素迁移是斜坡失稳孕育过程中显著的伴生作用,直观、细致地反映出斜坡失稳演化过程的长期、复杂、受多种因素控制的特征。Along with rockforming minerals weathering and secondary minerals formation, the shift of elements takes place. In shallow hypergene zone, the shift of elements is of long--term and complicated feature and is influenced by a lot of factors, which plays an important role in destabilization of slope.

关 键 词：元素迁移 风化壳 垂直分带 斜坡失稳 

分 类 号：P311.2[天文地球—固体地球物理学]