摘要
长宁梅硐石林位于扬子地台区西部边缘,由竹石林、石陇坡和天门寨三个景区组成,以奥陶系宝塔组龟裂纹灰岩岩溶石林与竹林共生为特色,具有独特的观赏价值和科学价值。根据研究区岩溶地貌的形态特征及微观成因,划分出10种主要的岩溶地貌类型,并从控制岩溶地貌形成的构造条件、成景地层、自然地理等方面对石林的成因和形成演化过程进行了简要的分析和总结。
The Meidong Stone Forest Geopark in Changning, Sichuan on the western margin of the Yangtze platform consists of three scenic spots such as Zhushilin, Shilongpo and Tianmenzhai which are characterized by karst stone forest from parched limestone of the Ordovician Baota Formation with bamboo forest. This paper divided the karst landform into 10 types and makes an approach to genesis and evolutionary process of the stone forest in terms of stratigraphy, tectonism and physical geography.
出处
《四川地质学报》
2012年第2期250-253,共4页
Acta Geologica Sichuan
基金
长宁梅硐石林地质遗迹调查
关键词
梅硐石林
成因
地质遗迹
长宁
Meidong Stone Forest
genesis
geopark
Changning
