1) last deglaciation
末次冰消期
1.
Paleoenvironmental Evolution in the Inner Shelf of the East China Sea Since the Last Deglaciation
末次冰消期以来东海内陆架古环境演化
2.
A typical borehole P5 was examined for lithology, dating, spore-pollen and microfossil to reveal the phases of climate and sea level fluctuation and the associated sedimentary facies recorded in the paleo-incised valley sediments in the southeastern Changjiang Delta Plain since the last deglaciation.
利用典型钻孔P5孔沉积物的岩性、测年、孢粉和有孔虫的分析结果,探讨了末次冰消期以来长江三角洲东南部古河谷区记录的气候波动和海平面阶段性上升过程及其控制下的古河谷沉积模式。
3.
The rapid climatic changes occurred at the northwest margin of East Asia monsoon region during the last deglaciation were divided into six climatic periods, namely Oldest Dryas, Exiling, Older Dryas, Allerd, IACP and Young Dryas periods.
通过对中卫剖面和米浪沟湾剖面的年代学与高分辨率气候地层记录的研究,认为末次冰消期东亚季风区西北缘发生气候快速变化事件,它可分辨出古仙女木、波令、老仙女木、阿勒鲁德、IACP 和新仙女木等6个气候阶段,并可与格陵兰冰心(GISP2)检出的6个气候阶段相对比。
2) the last deglaciation
末次冰消期
1.
On the basis of biological, lacustrine and glacial sediment stratigraphy records, the paper analyzed the features of climate change during the last deglaciation in the Tibetan Plateau, and correlated to the climatic evolution sequences in Europe and Greenland.
根据生物、湖泊及冰川地层记录,分析了青藏高原末次冰消期的气候演化特点,并将其与格陵兰、欧洲气候演化序列进行了对比分析。
2.
This paper reports a recent research on climatic and environmental evolution at Changgouzhen(38°32′N,115°47′E)area,60km southwest of Beijing city during the Last Deglaciation.
对北京房山县长沟镇附近埋藏末次冰消期湖沼沉积物层序和岩性变化的观测资料，以及１４Ｃ测年、孢粉分析、磁化率、有机碳δ１３Ｃ值和有机质含量等测定资料的综合研究表明：１）约１３０００ａＢ。
3.
The mud area off Yangtze River estuary is one of the accumulative centers of Yangtze River sediment since the last deglaciation transgression, the core ECS-0702 (122°40.
长江口滨外泥质区是末次冰消期海侵以来的长江入海物质沉积中心和“物质汇”之一,论文对取自该泥质区的ECS-0702孔(122°40。
3) last glaciation
末次冰期
1.
An intensive erosion event in the last glaciation in the west of China;
中国西部末次冰期一次强烈的侵蚀事件
2.
The Discovery of Sand Wedges of the Last Glaciation in the Hexi Corridor and Its Paleoclimatic Significance;
河西走廊末次冰期砂楔的发现及其古气候意义
3.
By means of the field investigation and experimental analysis in the laboratory, especially based on the absolute ages, the authors confirm the glacier evolution series of the last glaciation in Gongwangshan Mountain.
通过野外调查和室内试验数据综合分析 ,确定了拱王山末次冰期以来的冰期演化序列 ,认为本区末次冰期的时代分别为倒数第二次冰期 ,TL 年代为 10～ 11万年 ;末次冰期早期 ,4～ 5万年 ;末次冰盛期 ,1。
4) last glacial
末次冰期
1.
Paleo-environment of southern South China Sea since last Glacial:Evidence from planktonic foraminifera of core YSJD-86GC;
南海南部末次冰期以来的古环境变化:YSJD-86GC柱样的证据
2.
Study on the High-resolution Sequence of Vegetation Change During the Last Glacial Recorded in the Loess of Xishan Moutain of Beijing Area;
末次冰期北京西山黄土中高分辨率的植被演化过程研究
3.
And it also suggested that the climate in the East Asian Monsoon region had rapid fluctuations in millennium to century scales in the whole last glacial.
暗示在整个末次冰期,东亚季风气候同样存在千年—百年尺度上的快速波动。
5) last glacial age
末次冰期
1.
Study on the climatic changes between the last interglacial age and the last glacial age recorded by ostracoda in eastern Qaidam Basin;
末次间冰期—末次冰期柴达木盆地东部气候演化形式
2.
At least in the beginning of the last glacial age, the faices belts of dune sand, sandy clay and loess differentiated by the wind and aligned from north to south had already existed in the Taklimakan Desert and areas to its south.
至少在末次冰期初,塔克拉玛干沙漠及其以南就已存在风成的砂丘砂、亚砂土和黄土岩相带。
6) last ice age
末次冰期
1.
Mineral characteristics and their environmental implication during the last ice age in Core Q43 on the outer shelf of the East China Sea;
东海外陆架Q43岩心末次冰期矿物学特征及其古环境意义
2.
Tracing the Changjiang River s flowing route entering the sea during the last ice age maximum;
末次冰期盛期长江入海流路探讨
3.
The 14 C dating of eolian sands in sand wedges proves they formed during the Last Ice Age,with the mean annual air temperature about -5 6℃.
河西走廊砂楔主要形成在晚更新世冲洪积砾石层中 ,楔体内充填的风成砂14 C年龄证明其是末次冰期的产物 ,古砂楔所对应的年均气温为- 5 6℃左右。
补充资料：冰消
1.亦作"冰销"。 2.冰冻消融。 3.比喻事物消释涣解。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条