%0 Journal Article
%T SEDIMENTARY AND CLIMATIC SIGNIFICANCE OF THE STRATIFIED SLOPE DEPOSITS IN THE EARLY PERIOD OF LAST GLACIATION AT KUNLUNSHAN PASS<br>昆仑山垭口小南川末次冰期早期成层坡积的沉积特征和气候意义
%A Liu Gengnian
%A Cui Zhijiu
%A Ge Daokai
%A <br>刘耕年
%A 崔之久
%A 葛道凯
%A 伍永秋
%J 地理学报
%D 1997
%I 
%X 成层坡积结构构造特征、粒度、化学、电镜扫发描分析和测年资料揭示其形在于末次冰期间冰段（６００００ａＢＰ～４４０００ａＢＰ）。存在由湿冷向干冷的气候变化。成层坡积上覆的坡积黄土则代表末次冰期全盛及全新世环境以显著干冷为特征。此剖面突出表明昆仑山垭口地区末次冰期早期不是干冷，而是湿冷，与季风模式不吻合。故只能认为当时该区受西风带影响。
%K Kunlunshan Pass
%K Stratified slope deposits
%K Last Glaciation Cold
%K wet<br>昆仑山垭口，成层坡积，末次冰期，湿冷
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=869B153A4C6B5B85&jid=F7B5B947C24B9D649491012214E4BEF4&aid=BC37D20DA48C3235&yid=5370399DC954B911&iid=E158A972A605785F&journal_id=0375-5444&journal_name=地理学报&referenced_num=5&reference_num=0