Quaternary Geological Features of Beijing Piedmont Plain Using 3-D Structural Method <?xml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" /><o:p></o:p>

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Quaternary Geological Features of Beijing Piedmont Plain Using 3-D Structural Method

详细信息

责任者：Cai Xiangmin （Beijing Bureau of Geology and Mineral Resources Exploration and Development ; Beijing 100050 ; China） ; Guo Gaoxuan
刊名：Acta Geologica Sinica
出版年：2009
卷期：83(7)
关键词：第四纪 ; Quaternary ; 工程地质勘察 ; engineering geological investigation ; 北京 ; Beijing
页码：p.1047-1057
图表：7 illus., 1 table, 15 refs.
分类号：1400
issnNo：ISSN0001-5717
isbnNo：CN11-1951/P

摘要

With China’s urbanization speeding up, increasing urban construction such as city water supply, utilization of underground space resources, ground improvement, garbage disposal are closely related to geological work. Especially, metropolitan cities building on the Quaternary are being threatened from earthquake, active faulting, land subsidence, water shortage, scarce land, environmental deterioration, etc. Beijing, as one of the few gigantic metropolitan cities around the world, has no exception. But the subsistence and development of these cities are indispensable to the Quaternary unconsolidated sediments. Therefore, it is essential to understand the 3-D geologic structures of the Quaternary, because it will provide detailed spatial distribution data of geological bodies so as to prevent and reduce the occurrences of above-mentioned disasters.

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