摘要
李四光教授在庐山划分出三个冰期与两个间冰期，后来加上晚更新世的大理冰期，为四个冰期三个间冰期。李承三教授继而在四川西北部山区划分出五个冰期与四个间冰期。孙殿卿教授等后来在河北省泥河湾划分出六个冰期与五个间冰期。景才瑞等也曾在庐山与鄂西高原地区划分出四个冰期与三个间冰期。学者们比较公认的为：鄱阳冰期、鄱阳－大姑间冰期、大始冰期、大姑－庐山间冰期、庐山冰期、庐山－大理间冰期与大理冰期。目前处在冰后期。
Professor Li Siguang is one of the most earliest scientists who discovered that there were not only glacial stages, but also interglacial stages in China. At first, three glacial stages and two interglacial stages were divided from Lushan, and lately, the Dali glacial stage in late Pleistocene was discovered. So, there are four glacial stages and three interglacial stages in China. Five glacial stages and four interglacial stages were divided by Professor Li Chengshan from the northwestern Sichuan plateau. Six glacial stages and five interglacial stages were discovered by Professor Sun Dianqing in Nihewan of Hebei Province. Four glacial stages and three interglacial stages were divided by Jing Cairui from Lushan and the western Hubei plateau. In general, there are four glacial stages and three interglacial stages in Quaternary of China. They are Poyang glacial stage, Poyang Dagu interglacial stage, Dagu glacial stage, Dagu Lushan interglacial stage, Lushan glacial stage, Lushan Dali interglacial stage, and Dali glacial stage. Today is still in postglacial stage.
出处
《成都理工学院学报》
CSCD
1999年第1期97-100,共4页
Journal of Chengdu University of Technology
关键词
中国
第四纪
冰期
间冰期
地层
China
Quarternary
glacial stage
interglacial stage
