北京石花洞岩溶景观特色及成因探讨  

KARST LANDSCAPE FEATURES AND GENESIS OF BEIJING SHIHUADONG CAVE

作　　者：傅迷[1] 张文昭[1] 王俊辉[1] 唐洁云[1] 许新路[1] 黄文辉[1] 

机构地区：[1]中国地质大学能源学院,北京100083

出　　处：《资源与产业》2010年第6期149-155,共7页Resources & Industries

基　　金：北京市大学生科技研究与创新行动建设项目

摘　　要：北京石花洞地质公园区内地貌类型属典型的中低山构造剥蚀地貌,在碳酸盐岩沉积分布区经长期风化剥蚀和地表水的切割溶蚀,形成了较典型的岩溶地貌形态。在全国范围内,北京石花洞的层数最多,洞穴钟乳石种类齐全,毛细渗透水沉积的石花美丽,裂隙渗透水沉积的石盾最多、体积最大,滴水沉积的石笋叠置关系最明显,流水沉积的石旗发育奇特,池水沉积的月奶石发育最好,全新世石笋微层理发育最清晰。本文主要讨论石花洞岩溶景观成因,是本小组对石花洞进行的一次大体沉积类型研究。Beijing Shihuadong Cave Geopark has a typical low hill erosion terrain, which a long term of erosion and surface water cutting formed a characteristic karst terrain. Beijing Shihuadong cave ranks top in levels in China with all kinds of cave stalactites, and precipitating stone flowers through fine penetrating water, and precipitating stone shields through fissure penetrating water which are most in quantity and biggest in volumes. The stone shoots have a clear overlapping. Fancy in stone flags formed by currents, beautiful in stone moon precipitated by pool water, clear in the Holoeene stone shoots micro-bedding. This paper discusses the genesis of the karst cave and studies its sedimentary type.

关 键 词：岩溶地貌特色 地质成因 科学开发价值 北京 

分 类 号：P931.5[天文地球—自然地理学]