首页 | 本学科首页   官方微博 | 高级检索  
     检索      

延怀盆地晚更新世中晚期湖泊发育与气候变化
引用本文:郑荣章,计凤桔,李建平.延怀盆地晚更新世中晚期湖泊发育与气候变化[J].地震地质,2001,23(1):55-62.
作者姓名:郑荣章  计凤桔  李建平
作者单位:中国地震局地质研究所,
基金项目:中国地震局“九五”重点项目! (编号 950 4 10 0 6)资助
摘    要:延怀盆地晚更新世发育湖相沉积。根据 4个中晚期湖相层剖面的孢粉分析鉴定结果 ,结合区内晚更新世湖相层的年代测定及湖泊发育的分期 ,恢复了发育于 55~ 2 6和 2 0~ 8kaB .P .时间段内的第 2 ,3期湖泊发育期间的古气候环境。延怀盆地晚更新世中晚期湖泊沉积反映了潮湿气候的特征

关 键 词:延怀盆地  湖泊发育  孢粉分析  古气候
修稿时间:2000年9月1日

LAKE DEVELOPMENT AND CLIMATIC CHANGES, DURING THE MIDDLE AND LATE TIMES OF LATE PLEISTOCENE IN THE YANHUAI BASIN
Zheng Rongzhang,Ji Fengju,Li Jianping.LAKE DEVELOPMENT AND CLIMATIC CHANGES, DURING THE MIDDLE AND LATE TIMES OF LATE PLEISTOCENE IN THE YANHUAI BASIN[J].Seismology and Geology,2001,23(1):55-62.
Authors:Zheng Rongzhang  Ji Fengju  Li Jianping
Abstract:There was lake development during late Pleistocene in the Yanhuaibasin. On the basis of the results of sporopollen sample ananlyses for four profiles of the middle and late times of late Pleistocene in the basin, combined with dating of the lacustrine stratum and the stages of lake development, we have restored the paleoclimatic environment during 55~26ka B.P. and 20~8ka B.P., during which the second and the third period lacustrine stratum developed. The lake sediment of the middle and late time of late Pleistocene reflects a wet climatic characteristic of the Yanhuai basin.
Keywords:Yanhuai basin    Lake development  Sporopollen analysis    Paleoclimate
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号