晚冰期 meaning in Chinese
kataglacial
late glacial
Examples
- Late - glacial and holocene climate change recorded in loess profile in weibei loess tableland
渭北旱塬黄土记录的晚冰期以来短尺度气候变化 - Paleoclimatic and paleoenvironmental evolution since the late glacial epoch as recorded by sporopollen from the hongyuan peat section on the zoig 234 ; plateau , northern sichuan , china
川北若尔盖高原红原泥炭剖面孢粉记录的晚冰期以来古气候古环境的演变 - This work carries out a temporal - spatial analysis and comparison in facial pattern , grain - size , and susceptibility of the sediments of the hunshandake sandy land ( hsl ) on the basis of studies of more than fifty geological sections , a number of samples collected from surface sands as well as results derived from previous studies . the preliminary results of this work provide new environmental information of the working area , which makes it possible to have a brief discussion about the evolution of the hsl since the late glacial epoch . this work can be summarized as the followings
晚冰期,浑善达克沙地全面扩张,达到了沙漠化最大规模,剖面中的古风成砂是最直接的证据,此时气候干冷;全新世早中期,浑善达克沙地成壤比较好,是一个大面积成壤期,相当于全新世适宜期,此时气候暖湿;全新世晚期,浑善达克沙地沙漠化正过程加强,在沙地各剖面上普遍发育风沙沉积,气温较干冷;目前:浑善达克沙地为另一成壤期,成壤作用相对于适宜期较差,气候干暖。