河南跑马岭地质公园岩溶地貌特征  

Karst geomorphological characteristics in Paomaling geopark,Henan Province

作　　者：杨涛 宋利睿[2] 于增宝 

机构地区：[1]河南省地球物理工程勘察院,河南郑州450000 [2]河南省地质测绘总院,河南郑州450000

出　　处：《资源调查与环境》2009年第2期149-156,共8页Resources Survey & Environment

基　　金：河南省两权价款专项资金(2007-394)资助

摘　　要：河南跑马岭地质公园地处太行山东南麓,是一座以碳酸盐岩地质地貌为主题的地质公园。公园在不同的标高、地层层位和岩性等背景下,发育了不同的岩溶地貌。在查明公园岩溶地貌形态的基础上,对各种形态岩溶形成诸因素进行了统计、分析、和研究,总结了岩溶发育的规模、分布规律、含水量、洞内景观、地壳运动性质等,这些调查成果可作为进一步开发和规划的基础资料,对实现地质公园的可持续发展具有重要的现实意义。Located in the southeast of Taihang Mountain, Henan Province, the Paomaling geop- ark has a subject of carbonate geomorphological landscapes. In the background of different elevations, stratigraphic horizons and lithologic characters, different karst landforms are developed. In this article, on the basis of investigation of karst geomorphological charac- teristics, statistics, analysis and research on different factors for the formation of different morphological karsts have been carried out, and development scale, distribution regulari- ty, water content, landscape in the karst cave, crustal movement and others also have been summed. These investigation results can be used as the basic data for the further de- velopment and planning of karst landscapes and have a great realistic significance for the sustainable development of the geopark.

关 键 词：跑马岭 地质公园 岩溶地貌 河南 

分 类 号：P931.5[天文地球—自然地理学]