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云南黎明高山丹霞地貌成因及其演化模式
引用本文:杨洪玉,杨艳华,白光顺.云南黎明高山丹霞地貌成因及其演化模式[J].云南地质,2011,30(3):370-372.
作者姓名:杨洪玉  杨艳华  白光顺
作者单位:1. 昆明理工大学国土资源工程学院,云南昆明,650093
2. 云南地质环境监测总站,云南昆明,650000
摘    要:始新统红色磨拉石建造和裂隙网奠定黎明丹霞地质景观条件,岩石中富含各种致色元素,使丹霞峰林赤壁呈现多种颜色;内外动力共同作用,形成黎明地区分布范围广、极具独特性的高山丹霞地貌单体形态和组合形态。高山丹霞地貌的形成与演化,可分为四个主要阶段。

关 键 词:高山丹霞地貌  内外营力作用  成因条件  四阶段演化模式  云南黎明

THE GENESIS AND EVOLUTION MODEL OF HIGH MT DANXIA GEOMORPHOLOGY IN LIMING, YUNNAN
YANG Hong-yu,YANG Yan-hua,BAI Guang-shun.THE GENESIS AND EVOLUTION MODEL OF HIGH MT DANXIA GEOMORPHOLOGY IN LIMING, YUNNAN[J].Yunnan Geology,2011,30(3):370-372.
Authors:YANG Hong-yu  YANG Yan-hua  BAI Guang-shun
Institution:YANG Hong-yu1,YANG Yan-hua2,BAI Guang-shun1(1.College of Land Resource Engineering,Kunming University of Science & Technology,Kunming 650093)(2.Yunnan Supervision Station of Geological Environment,Kunming 650000)
Abstract:The conditions of Liming Danxia geomorphological landscape are founded on Eocene red molasse formation and fissure net. Because of the variation coloration elements in rocks, the red cliff of Danxia peak forest shows variety of colors. Owing to the process of inner and outer dynamics of red bed altogether, the individual and composite states of the broad and very distinctive high Mt Danxia Geomorphology are formed, which can be divided into 4 main stages.
Keywords:High Mt Danxia Geomorphology  Genesis  Evolution Model  Liming  Yunnan
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