滇中轿子山地区地貌结构与特征研究  

LANDFORM SYSTEM STRUCTURES AND CHARACTERISTICS OF THE JIAOZI MOUNTAIN AREAS IN CENTRAL YUNNAN PROVINCE

作　　者：苏骅[1] 王平[2] 徐强[2] 

机构地区：[1]保山学院资源环境学院,云南保山678000 [2]云南师范大学旅游与地理科学学院,云南昆明650092

出　　处：《云南地理环境研究》2013年第3期19-23,共5页Yunnan Geographic Environment Research

基　　金：云南省林业厅"轿子山自然保护区综合科学考察项目"

摘　　要：通过野外实地考察地质结构、地貌发育及室内实验的方法,对滇中轿子山地区地貌结构和发育特征进行了分析,对轿子山及其外围山地的喀斯特地貌、古冰川遗迹及冻土地貌进行了研究。结果表明:轿子山地区主要构造形迹为褶皱与断裂,轿子山地区整体地势中部高,向东西两侧呈阶梯状下降,河谷切割较深,相对高差大,区内构造地貌发育,地貌大格局受构造控制明显,构造地貌、玄武岩台地、灾害地貌、第四纪冰川遗迹残广布,古冰川遗迹冻土地貌较为发育。Through the visits landform structures and landform development and laboratory experiments. Analysis the Jiaozi Mountain landform structure and developmental characteristics. Study the karst, ancient glaciers and permafrost landforms of Jiaozi Mountain. The results show that： main structure acting of Jiaozi Mountain as folds and fracture. The Mountain is Central high surrounded by low, the Valley cutting deep, relatively large height difference. The tectonic geomorphology development in the region, landform pattern of apparent structural control, Quaternary glacial remains residual widespread and the ancient glaciers permafrost landforms is more developed.

关 键 词：轿子山 地貌结构 地貌特征 

分 类 号：P931[天文地球—自然地理学]