鄂西南岩溶旅游资源成因及成景模式分析  

Study on the origin and evoluting patterns of karst tourist resources in southwest Hubei

作　　者：徐松华[1] 

机构地区：[1]武汉商学院旅游经济研究所,湖北武汉430056

出　　处：《商丘师范学院学报》2015年第9期84-88,共5页Journal of Shangqiu Normal University

基　　金：武汉商学院科学研究项目(2014Y009)资助

摘　　要：以鄂西南丰富的岩溶旅游资源为研究对象,从地质学、岩溶学和旅游学等多学科视角对其成因进行了探讨.指出该地区广泛出露的可溶性岩层是物质基础,多期地质构造是控制条件,岩溶作用是成景过程的关键性因素,以及气候、地形和植被是外动力因素.最后总结出了鄂西南岩溶旅游资源成景模式图.This paper regards Karst tourist Resources in Southwest Hubei as the research object,and analyzes its origin with the use of the geology,karst and tourism. Then concludes that abundant soluble rocks are the Material basis of its origin,Multiperiod Geological structure is the Controlling condition of its origin,Karstification is the key factor of its origin,Climate,topography and vegetation is outside dynamic factors of its origin. Finally this paper summarizes the diagram which demonstrates the formation and development of Karst tourist resources in Southwest Hubei.

关 键 词：鄂西南 岩溶作用 旅游资源 成因 成景模式 

分 类 号：K903[历史地理—人文地理学]