摘要
通过贵州省岩溶洼地实地考察分析,从地质学角度对岩溶洼地成因做了详细的归纳分析。提出了岩溶洼地地质成因有岩溶裂隙发育形成和地下河流岩溶塌陷形成两种,并对这两种不同成因类型的岩溶洼地地貌特征做了详细对比。
Through the field investigation and analysis of karst depression in Guizhou Province, the genesis thereof is generalized and analyzed in details from the viewpoint of geology. The two origins, including karst fissure development and karst collapse along underground river, are proposed and the geomorphic features of the karst depression caused therefrom are compared carefully.
出处
《路基工程》
2012年第6期23-26,共4页
Subgrade Engineering
基金
贵州省优秀青年科技人才培养专项资金项目(黔科合人字2009-23)
关键词
岩溶洼地
地质成因
岩溶裂隙
地下河流
karst depression
geological genesis
karst fissure
underground river
