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出 处:《云南地理环境研究》2010年第5期6-11,共6页Yunnan Geographic Environment Research
基 金:2010年福建省教育厅社会科学项目;福建省属高校项目(2008F50401);福建省社会科学基金项目(2009B2078)
摘 要:晚第三纪到第四纪的新构造运动,对福建省主要旅游资源自然基底的内部构造和外部形态都有深远影响。新构造运动背景下,福建省内国家AAAA级及以上等级旅游景区分布极不均匀,主要旅游资源集中在闽东沿海断块差异活动区和闽西断陷上升区,且有4个主要特征,即主要旅游资源多集中在断陷区,旅游景区可进入性较好、地文景观类旅游资源丰富,以中、低山为主、以政和-大埔断裂为界,东西两侧旅游资源各具特色、温泉旅游资源主要分布在闽江以南,温泉出露点海拔高度较低,以淡水、中高温泉为主。The Neotectonics,from Late Tertiary to Quaternary,has far-reaching implications on the internal structure and external morphology of the natural base in Fujian main tourism resources.Uder the background of Neotectonics,the distribution of national AAAA and AAAAA level scenic spots in Fujian Province is very uneven,and the main tourism resources concentrated in the difference block activity area of coastal,and the rift up area of western.There are four main features of the main tourism resources.Firstly,the main tourism resources concentrate in the fault depression area,and the tourism area has a good access.Secondly,there is rich landscape in the main tourism resources,and most of them are medium and low mountains.Thirdly,the characteristic of tourism resources in the east and west sides of Zhenhe-Dabu fault is distinctive.lastly,hot springs tourism resources,most of which are freshwater,high spring and low elevation,are mainly distributed in the south of Minjiang river.
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