期刊文献+

北京西山的冰缘期和更新世自然环境 被引量:12

Periglacial Periods and Pleistocene Environment in Western Mountain of Beijing, China
下载PDF
导出
摘要 根据已发现的若干古冰缘现象,北京西山可以划分为6次更新世冰缘期。在冰缘期期间,地表气温比现今低12—15℃;冬季固体降水量比现今大;多年冻土深度达-3—20m以上;自然环境为稀树草原或冻原。中国东部冰缘区南界达38°N。 Periglacial phenomena are widely distributed in Western Mountain of Beijing, China. This paper is the first report on the studies of some fossil periglacial phenomena in that region. Four kinds of fossil periglacial phenomena were found: ice wedges, periglacial involution, congelifolds and congelisolifluctive deposits. According to stratigraphical and chronological data, the periglacial periods have been divided as following: 1. Guanting periglacial period, characterized by the congelisolifluctive deposits developed in Shizhuang formation, with an age of 2.43 Ma B.P. from paleomagnetic dating; 2. Yanchi periglacial period, characterized by the congelifold developed in Yanchi formation, with an age of 0.5 Ma B.P. from pleomagnetic dating; 3. Zhaitang periglacial period(Ⅱ), characterized by the periglacial involution developed in Zhaitang formation, with an age of 0.3 Ma B.P. from paleomagnetic dating; 4. Zhaitang periglacial period( Ⅰ ), characterized by the ice (soil) wedge developed in Zhaitang formation, with an age of 0.2 M a B.P. from paleomagnetic dating; 5. Qiansangyu periglacial period(Ⅱ), characterized by the ice (sand) wedges developed in Qiansangyu formation, with an age of 0.13 Ma B.P. from paleomagnetic dating; 6. Qiansangyu periglacial period( Ⅰ), characterized by the ice (soil) wedge developed in Qiansangyu formation, with an age of 0.018 Ma B.P. from thermolunscent dating. These fossil ice wedges, periglacial involutions and congelifolds indicated a rather arid and windy periglacial environment with a mean annual temperature estimated to be some 12 -15℃colder than that at the present. During about 0.5-0.018 Ma B.P., the southern boundary of Pleistocene permafrost extended to the latitude 38°N. The depth of permafrost is about -3 m to -20 m, during Pleistocene periglacial periods. Finally, the problems on vegetations, precipitation etc. were discussed.
出处 《冰川冻土》 CSCD 北大核心 1991年第2期159-167,共9页 Journal of Glaciology and Geocryology
基金 中国科学院地质研究所科学基金
关键词 冰缘 更新世 自然环境 Pleistocene, periglacial phenomena, periglacial periods, natural environment
  • 相关文献

参考文献5

  • 1卢演俦,A.J.Mortlock,D.M.Price,M.L.Readhead.马兰黄土的粗颗粒石英热释光断代[J]科学通报,1988(01).
  • 2郭旭东.中国第四纪气候环境的初步研究[J]冰川冻土,1984(01).
  • 3谢又予.我国东北地区的冰缘地貌与分区[J]冰川冻土,1981(04).
  • 4郭旭东,严富华,叶永英,孙建中.从模式口“冰川遗迹”看北京西山区第四纪冰川作用发生的可能性[J]冰川冻土,1981(02).
  • 5孙建中.松辽平原冰缘期的划分[J]地理科学,1981(02).

同被引文献116

引证文献12

二级引证文献95

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部