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《Geological Bulletin of China》 2010-04
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Formation of karst cave system and its relationship with neotectonic movement in Beijing Western Hills,Beijing,China

L Jin-bo1,LU Yao-ru2,ZHENG Gui-sen3,ZHENG Ming-cun41. Beijing Geological Survey ,Beijing 102206,China; 2. Chinese Academy of Geological Sciences,Beijing 100037,China; 3. Beijing Bureau of Geology and Mineral Exploration and Development,Beijing 100195,China; 4. Management Committee of Scenic Spot of Shihua Cave in Fangshan District,Beijing 102416,China  
The strata formed karst in North China are mainly composed of Majiagou Formation in Ordovician and dolomite with siliceous bands of Wumishan Formation,Jixian System in Middle Proterozoic. The local Fangshan landform is made up of Pliocene stone forest on mountain top and Quaternary karst stone cliffs,all formed within Wumishan Formation. Karst caves are either developed in Majiagou Formation or Wumishan Formation. Shihua Karst cave system along the south bank of Dashi River consists of Jimao Cave,Yinhu Cave,Shihua Cave,Qingfeng Cave and Kongshui Cave,connected by an underground river. Shihua Cave system is developed on top of Majiagou Formation in northeast uplifting limb of Beiling syncline. There is Fangshan granodiorite between Shihua Cave system and another Karst Cave system of Peking Man Site at Zhoukoudian. Eight altitude levels of Shihua Cave system represent corresponding times of the neotectonic movement in Beijing Western Hills. It may correlate with Physiographic Stages of North China and terraces of Yongding River.
【Fund】: 北京市地质矿产勘查开发局项目(编号:dkjdzky20082001);; 北京市科学技术委员会项目(编号:855600400);; 中国地质调查局项目(编号:20001300005031)共同资助
【CateGory Index】: P512.2
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