摘要
山位于湖南新宁县城南12km，面积102．28km2，海拔300－818m。资水上游─扶夷江纵贯南北。山在早白垩纪前为剥蚀区，白里纪初期断陷为NNE向长条形山间盆地，并沉积了厚达200－2320m的紫红色碎屑岩系。第三纪盆地挤压回升，形成立斜断决山。在岩性、构造、气候、水文、时间等因素的综合影响下，山形成了复杂的地貌类型，为典型的丹霞地貌及优良的旅游资源。
Langshan is 12 Km far from XinLin corntoy town of Hunan Province,amd lies to south of the town It is 1O2 28 Km2 and 3OO-818 metersabove sea level. The up-per reach of the Zi River,Fuyi River, crossesfrom south to north. Lantshan was a de-nuded area before the earlycretaceous period. It was a Long badin between-mountain extendingalong NNE in the early Cretaceouss period. and it was extraded to be amonocli-nal fanlt mountain in the Tertiary period. Becaude of the multiple function of lithology,Condtructure, climate, hydrology and time, there are various types of landforms, typical red landforms and excellemt tourist resources in Langsha.
出处
《湘潭师范学院学报（社会科学版）》
1997年第3期65-71,共7页
Journal of Xiangtan Normal University(Social Science Edition)
基金
湖南省自然科学基金
关键词
茛山
地貌特征
丹霞地貌
旅游资源
Langsan
Characteristic of landforms
Rid landforms
Tourist redources
