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北京城市建设和发展的地质要素

Geological Elements for Urban Construction and Development of Beijing World City
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摘要 北京位于欧亚大陆东部,太平洋西岸,北纬40°,东经116°附近,是具有山区、平原和盆地的城市,是世界上具有地热资源的6个首都之一。目前,北京有1个世界地质公园、6个世界文化遗产地。其中,有以喀斯特景观为特色的房山石花洞世界地质公园;横亘于北山火成岩上的古代万里长城;位于温榆河下游两大洪积扇之间的古运河;房山周口店"北京人"遗址等等。 Located in the east of Eurasia and the geographic location near 40°N, 116°E, Beijing is an unwonted city in the world, including mountainous area, plain and basin. It is one of the six capitals with geothermal resources. It is also the junction of the Great Wall and Beijing-Hangzhou Grant Canal. At present, there are one global geopark and six world cultural heritages in Beijing. Of them, Fangshan Global Geopark is famous for the karst landscape; The Great Wall is on igneous rocks of Yanshan Mountain; Zhoukoudian Peking Man Site is in Fangshan Global Geopark. Summer Palace is a landscape of lake and mountain formed by Ordovician System and Permian System. Ming Tombs are in karst basin composed of Proterozoic marine facies sedimentary rocks. Imperial Palace is in middle of Yongding River Alluvium and Proluvium Fan. Heaven Temple is in overflow of the Fan. Beijing has been as a World City on Eurasia since Yuan Dynasty, and it was also the city which Christopher Columbus had looking for in his lifetime. Between Yongding River Fan and Chaobai River Fan, Wenyu River is the best layout center line to let Beijing be a World City.
作者 吕金波
出处 《城市地质》 2011年第2期8-11,34,共5页 Urban Geology
关键词 世界城市 温榆河规划中心线 房山世界地质公园 世界文化遗产 Beijing World City Layout center line of the Wenyu River Fangshan Global Geopark Worldcultural heritage
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