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机构地区:[1]Karst Research Institute ZRC SAZU,Titov trg 2,6230 Postojna,Slovenia
出 处:《Acta Geologica Sinica(English Edition)》2010年第2期424-431,共8页地质学报(英文版)
基 金:supported by Slovenia's Ministry of Higher Education,Science and Technology(Slovenian Research Agency),and China's Ministry of Science and Technology. included in the IGCP projects 448 and 513
摘 要:Mushroom Mountain karren with predominantly flat tops that formed along the stylolites and bedding planes dictated the special features of this karst landscape. Their features and rock relief clearly reflect the geological conditions and development. The subsoil karren with conical tops dissected by subsoil rock relief were exposed from beneath the soil. Below tree vegetation, the subsoil karren are to a great extent covered by moss and lichen, under which they acquire their characteristic shape. On the bare surface they were reshaped by rainwater that carves flutes and solution pans. The old cave that opens below the top of one of the cones reveals the period before its dissection into hills and cones when this part of the karst aquifer was still deep under the water table.Mushroom Mountain karren with predominantly flat tops that formed along the stylolites and bedding planes dictated the special features of this karst landscape. Their features and rock relief clearly reflect the geological conditions and development. The subsoil karren with conical tops dissected by subsoil rock relief were exposed from beneath the soil. Below tree vegetation, the subsoil karren are to a great extent covered by moss and lichen, under which they acquire their characteristic shape. On the bare surface they were reshaped by rainwater that carves flutes and solution pans. The old cave that opens below the top of one of the cones reveals the period before its dissection into hills and cones when this part of the karst aquifer was still deep under the water table.
关 键 词:KARST karren CAVE rock relief development of karst Shizong YUNNAN
分 类 号:P542[天文地球—构造地质学]
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