河北省临城白云洞景观成因类型  

The Genetic Types of Baiyun Cave in Lincheng County,Hebei Province

作　　者：孙艳萍[1] 王健[1] 张小曼[1] 郑倩华[1] 黄华芳[1] 

机构地区：[1]河北师范大学/河北省环境演变与生态建设实验室,石家庄050016

出　　处：《湖北农业科学》2013年第7期1541-1545,共5页Hubei Agricultural Sciences

基　　金：国家自然科学基金重点项目(40730103)

摘　　要：河北省临城白云洞是我国北方半湿润气候条件下发育形成的罕见溶洞,发育于早古生代中寒武统张夏组碳酸岩为主的地层,洞内侵蚀-溶蚀景观和化学沉积景观类型十分丰富,形态多样,具有石幔、石旗、石盾、石钟乳、石笋、石花、石葡萄、鹅管等景观,尤以卷曲石、鹅管、石花等景观最具特色。Baiyun Karst Caverns in Lincheng county,Hebei province,is a rare karst caverns in subhumid climate region of the north.It was developed in carbonatite strata,particularly in Zhangxia formation of the Middle Cambrain series.Erosioncorrision landscape and chemical deposition landscape are very abundant.They are in various shapes,have the landscapes of curtain drapery,cave flag,cave shield,stalactite,stalagmite,cave flowers,botryoid and soda straw,especially heligmite,soda straw,cave flowers are the most characteristic landscapes.

关 键 词：临城白云洞 景观 成因类型 

分 类 号：S[农业科学]