Evolvement of Karst Landform in Shenglianshan Geopark in Western-Hill, Beijing
详细信息
- 责任者：Lv Jinbo (Beijing Geological Survey ; Beijing 102206 ; China) ; Liu Zengli
- 刊名：City Geology
- 出版年：2011
- 卷期：6(3)
- 关键词：地质公园 ; geological park ; 岩溶地貌 ; karst features ; 北京 ; Beijing
- 页码：p.22-27,39
- 图表：13 illus., 11 refs.
- 分类号：1400
- 出版序号：20122612
- issnNo：ISSN1007-1903
- isbnNo：CN11-5519/P
摘要
There is a small-scale karst basin in Dashi upriver in north of Fangshan District, Beijing. Shenglianshan Geopark is located at Fangshan Global Geopark; to geological structure, it is situated at the south of Baihuashan syncline. From the bottom up, the sedimentary rocks are oolitic limestone of Cambrian Zhangxia Formation, stripe limestone of Cambrian Chaomidian Formation and limestone of Ordovician. In the geological history, three staged movements of Indosinian Movement, Yanshanian Movement and Neotectonic Movement have formed the beautiful landscapes in the geopark. The Xiangshan anticline was formed by the convergence from Indosinian Movement.