中国岩溶旅游资源空间格局  

Spatial Pattern of Karst Tourism Resources in China

作　　者：韦跃龙[1,2] 陈伟海[2] 黄保健[2] 覃建雄[1] 

机构地区：[1]成都理工大学地球科学学院,成都610059 [2]中国地质科学院岩溶地质研究所,广西桂林541004

出　　处：《桂林工学院学报》2008年第4期473-483,共11页Journal of Guilin University of Technology

基　　金：广西科学研究与技术开发计划资助项目(桂科攻0719005-1)

摘　　要：中国岩溶旅游资源类型丰富,分布于不同的岩溶区域,具有集中性、差异性和地区性等空间分布特征。按地理和行政区域及系统分区分类的方法,将中国岩溶区域分为4级:区域、区、亚区和样块,并以岩溶景观的山景、水景、洞景等3种主要类型来分析、总结和概括各岩溶区的景观异质性、组合特征、特色等。认为岩溶景观发育过程是沉积过程、岩溶过程、构造运动和气候变化的统一复合体,是一个富反馈的系统,在影响和控制岩溶景观发育的各因素之间存在着复杂的反馈关系并构成一个动态、复杂的岩溶景观成景耦合系统,它们共同的作用对象是成景地层,通过不同的物理、化学和生物过程来完成。通过分析总结认为各岩溶区域成景耦合系统间的差异是造成中国岩溶旅游资源空间异质性的根本原因。Karst tourism resources in China are abundant, and distributed in different karst areas with these characters of centrality, otherness and territory. According to geography, regionalism subarea and classes of system, karst tourism resources in China are identified into four grades ： area, region, subregion, and sample （ national park or geopark, among which karst landscape dominates）. From three karst landscape primary types, mountain scape, water scape, hole scape, the scape difference, its assembled character, and the feature of every karst region are analyzed. The developing process of karst landscape is considered to be a uniform synthesis and a feedback system throngh the process of sediment, the process of karst, tectonic movement and climate changes. There is complicated feedback relation among these four factors, with a dynamic, complicated and coupled system of the formation of karst landscape. The collective object mentioned above is stratum, and the sight formation is finished by different process of physics, chemistry and biology. Based on the analysis the coupled system of the formation of karst landscape in different area causes the karst difference in China.

关 键 词：岩溶旅游资源 空间格局 岩溶景观 成景耦合系统 

分 类 号：P642.253[天文地球—工程地质学]