Genesis and Evolution of Kongshan Baiyun Karst Cave in Lincheng County, Hebei Province
Received date: 2012-07-03
Revised date: 2012-11-05
Online published: 2013-01-10
Kongshan Baiyun karst cave system in Hebei Province developed mainly in Carbonate strata of Middle Cambrian Zhangxia Formation. The horizontal distribution of the karst cave system was controlled by NNW, NE, and nearly EW faults. Baiyun karst cave system can be divided into three layer caves vertically, and every layer cave was connected by the passages which formed by erosion and corrosion following the steep faults. The first layer hall-like caves (paradise, the human world and netherworld) which developed along NNW faults formed in the mid-late stage of Early Pleistocene. The second layer reticula caves (maze and upper dragon palace) which developed tracking NNW and NE faults formed from the middle stage of Middle Pleistocene to the beginning of Late Pleistocene. The third layer zigzag Corridorshape caves (lower dragon palace) following NE and NNW faults formed during the late of Late Pleistocene to the beginning of Early Holocene. Baiyun karst caves were damaged repeatedly by tectonic movements during the development of them. Nowadays, the disaster bearing capacity of Baiyun karst caves are very low. Therefore, protecting the cave structure stability and controlling the geological environment are important work at present.
Zheng Qianhua , Wang Jian , Zhang Xiaoman , Sun Yanping , Huang Huafang . Genesis and Evolution of Kongshan Baiyun Karst Cave in Lincheng County, Hebei Province[J]. Advances in Earth Science, 2013 , 28(1) : 86 -93 . DOI: 10.11867/j.issn.1001-8166.2013.01.0086
[1]Chen Weihai. An outline of speleology research progress[J]. Geological Review,2006, 52(6): 783-792.[陈伟海. 洞穴研究进展综述[J]. 地质论评, 2006, 52(6): 783-792.]
[2]Yuan Daoxian. Karst in southwest China and its comparison with karst in North China[J]. Quaternary Sciences, 1992, (4): 352-361.[袁道先. 中国西南部的岩溶及其与华北岩溶的对比[J].第四纪研究, 1992, (4): 352-361.]
[3]Song Linhua. Progress and trend of Karst geomorphology study[J].Progress in Geography, 2000, 19(3): 193-202.[宋林华. 喀斯特地貌研究进展与趋势[J]. 地理科学进展,2000, 19(3): 193-202.]
[4]Jiang Zhongcheng, Pei Jianguo, Xia Riyuan, et al. Progresses and important activities of Karst research during the 11th Five-Year Plan in China[J]. Carsologica Sinica, 2010, 29(4): 349-354.[蒋忠诚, 裴建国, 夏日元, 等. 我国“十一五”期间的岩溶研究进展与重要活动[J]. 中国岩溶, 2010, 29(4): 349-354.]
[5]Ren Qingguo. Formation and evolution of Kongshan Baiyun Karst Cave, Lincheng County[J]. Journal of Xingtai University, 1990, (2): 45-48.[任庆国. 临城县崆山白云洞的形成与演化[J]. 邢台地区教育学院院报, 1990, (2): 45-48.]
[6]Peng Yimin, Zhao Huaxin. Evaluation and exploitation of tourism geologic resource of Baiyun Karst Caverns in Lincheng County, Hebei Province[J].Journal of China University of Geosciences (Earth Science),1994, 19(2): 262-271.[彭一民, 赵华新. 河北省临城县白云山岩溶洞穴旅游地学资源的评价与开发[J]. 中国地质大学学报:地球科学版, 1994, 19(2): 262-271.]
[7]Song Linhua, Sui Shuchun, Chen Gangling, et al. On the phenomenon of origination and weathering of speleothem in Baiyundong in Lincheng County of Hebei Province[J]. Geography and Territorial Research, 2000, 16(3): 68-74.[宋林华, 睢树春, 陈岗岭, 等. 河北省临城白云洞洞积石形成与风化现象研究[J]. 地理学与国土研究, 2000, 16(3): 68-74.]
[8]Song Linhua, Wei Xiaoning, Liang Fuyuan. Effect of speleo-tourism on the CO2 content and temperature in Baiyun Cave, Lincheng, Hebei[J]. Carsologica Sinica, 2003, 22(3): 230-235.[宋林华, 韦小宁, 梁福源. 河北省临城白云洞洞穴旅游对洞穴CO2浓度及温度的影响[J]. 中国岩溶, 2003, 22(3): 230-235.]
[9]Zhang Yuanhai, Chen Weihai, Deng Yadong. Genesis of Stalactite Relics on the top of Kongshan in Lincheng County, Hebei Province[C]∥Observations, Research, Development and Protection of the Caves: Selected Papers from National Cave Conference. Beijing: Geological Publishing House, 2008.[张远海, 陈伟海, 邓亚东. 河北临城崆山山顶钟乳石遗迹成因分析[C]∥洞穴观测、研究、开发与保护: 全国洞穴学术会议论文选集. 北京: 地质出版社, 2008.]
[10]Bureau of Geology and Mineral Resources of Hebei Province. Regional Geology of Hebei Province, Beijing Municipality and Tianjin Municipality[M]. Beijing: Geological Publishing House, 1989.[河北省地质矿产局. 河北省北京市天津市区域地质志[M]. 北京: 地质出版社, 1989.]
[11]Wu Chen. Discussion on formation times of the low piedmont surface in the mountain land of North China[J]. Geography and Geo-Information, 2004, 20(2): 105-108.[吴忱. 对华北低山麓面形成时代之新识[J]. 地理与地理信息科学, 2004, 20(2): 105-108.]
[12]Wu Chen. Landform Environment and Its Formation in North China[M]. Beijing: Science Press, 2008.[吴忱. 华北地貌环境及其形成演化[M]. 北京: 科学出版社, 2008.]
[13]Wang Hesheng. Floristic Geography of North China[M]. Beijing: Science Press, 1997.[王荷生. 华北植物区系地理[M]. 北京: 科学出版社, 1997.]
[14]Zhang Junhui, Xia Dunsheng, Zhang Ying, et al. Advances in palaeoclimatic research recorded by Peat in China since the Last Deglaciation[J]. Advances in Earth Science, 2012, 27(1): 42-51.[张俊辉, 夏敦胜, 张英, 等. 中国泥炭记录末次冰消期以来古气候研究进展[J]. 地球科学进展, 2012, 27(1): 42-51.]
[15]Pan Baotian, Gao Hongshan, Wu Guangjian, et al. Dating of erosion surface and terraces in the Eastern Qilian Shan, Northwest China[J]. Earth Surface Processes and Landforms, 2007, 32(1): 143-154.
[16]Gao Hongshan, Pan Baotian, Wu GuangJian, et al. Age and genesis of alluvial terraces in East Qilian Mountains[J]. Scientia Geographica Sinica, 2005, 25(2): 197-202.[高红山, 潘保田, 邬光剑, 等. 祁连山东段河流阶地的形成时代与机制探讨[J]. 地理科学, 2005, 25(2): 197-202.]
[17]Gao Hongshan, Pan Baotian, Li Jijun, et al. Age and genesis of the stepped geomorphic surfaces in Jinta River Basin of the Eastern Qilian Mountains[J]. Journal of Mountain Science, 2005, 23(3): 129-135.[高红山, 潘保田, 李吉均, 等. 祁连山东段金塔河流域层状地貌时代与成因探讨[J]. 山地学报, 2005, 23(3): 129-135.]
[18]Zhou Tingru. Changes of the natural environment in China during the Quaternary Time[J]. Scientia Geographica Sinica, 1983, 3(3): 191-206.[周廷儒. 中国第四纪古地理环境的分异[J]. 地理科学, 1983, 3(3): 191-206.]
[19]Zhou Kunshu. Pollen Analysis and Environmental Archaeology[M]. Beijing: Academy Press, 2002.[周昆叔. 花粉分析与环境考古[M]. 北京: 学苑出版社, 2002.]
/
| 〈 |
|
〉 |
甘公网安备62010202000687
