Glacial Maximum

美 [ˈɡleɪʃl ˈmæksɪməm]英 [ˈɡleɪʃl ˈmæksɪməm]
  • 网络冰川作用极盛期;最大冰期;最大冰川期
Glacial MaximumGlacial Maximum
  1. The Shift of Tropical Zone During The Last Glacial Maximum in China

    末次冰期盛期中国热带的变迁

  2. Analysis of Sea-Level Variation in the East China Sea Since the Last Glacial Maximum

    中国东海2万年来海平面变化分析

  3. Evolution and drought events in arid region of northern China since the last glacial maximum

    末次盛冰期以来中国北方干旱区演化及短尺度干旱事件

  4. A modeling research on East Asia monsoonal climate at the last glacial maximum

    末次冰期东亚季风气候的数值模拟研究

  5. Reconstruction of paleocoastlines for the northwestern South China Sea since the Last Glacial Maximum

    南海西北部末次盛冰期以来的古海岸线重建

  6. The last glacial maximum climate problem in the sea area of the Nansha islands , south China Sea

    南沙海区盛冰期的气候问题

  7. Desert Evolution and Climate Change of Southern Margin of Tengger Desert since Last Glacial Maximum

    腾格里沙漠南缘末次冰盛期以来沙漠演化与气候变化

  8. Sea-level rise and sedimentary environment response in the East China continental shelf since the last glacial maximum

    中国东部陆架沉积环境对末次冰盛期以来海面阶段性上升的响应

  9. An Overview of the Research on Channel Evolution in the Yangtze River Mouth Region Since the Last Glacial Maximum

    末次盛冰期以来长江河口段河道演变研究综述

  10. Paleoclimatic evolution deduced from organic carbon isotope of western Loess Plateau sediments since Last Glacial Maximum

    黄土高原西缘末次盛冰期以来古气候演化的有机碳同位素记录

  11. Preliminary study on the Climate Changes in the Processes of Regression before the Last Glacial Maximum in the Yangtze Delta Area

    长江三角洲地区末次冰盛期前海退过程中气候变化的初步研究

  12. Rapid climate variability recorded by mollusk species on the Loess Plateau during the last glacial maximum

    末次盛冰期黄土高原蜗牛化石记录的气候快速变化及其影响机制

  13. Grain-size characteristics of the first hard clay and their environmental implications during the last glacial maximum in the Hangzhou Bay region

    杭州湾地区末次冰盛期第一硬质黏土层粒度特征及其环境意义

  14. Comparison Between Nanjing Stalagmite δ ~ ( 18 ) O and Annual Layer Thickness Records During the Last Glacial Maximum

    盛冰期南京石笋δ~(18)O与年纹层厚度的对比

  15. Pollen-based reconstruction of vegetation in China during the mid-Holocene and last glacial maximum using a global scheme of plant functional types

    基于孢粉数据和植物功能型全球分类系统的全新世中期和末次盛冰期我国古植被格局定量重建

  16. Century-scale climatic oscillations during the last glacial maximum recorded in a stalagmite from Nanjing

    末次盛冰期百年尺度气候变化的南京石笋记录

  17. Oxygen and carbon stable isotopic records of planktonic foraminifers from the western equatorial Pacific since the last glacial maximum

    赤道西太平洋末次盛冰期以来的浮游有孔虫氧碳稳定同位素记录

  18. Variations in the eolian environment of North America during the last glacial maximum and their significance in the global abrupt climatic events

    末次盛冰期北美风成环境变化及其在全球气候突变事件中的意义

  19. Climate conditions in the Last Glacial Maximum ( LGM , 18 kaBP ) were remarkably different from the present .

    末次冰盛期(18kaBP)是两万年来距人类环境最近、与现代反差最大的气候时期。

  20. The discovery of palaeo eolian sand formed in the last glacial maximum and environmental evolution in the northwest of Shanxi

    晋西北地区末次盛冰期古风成砂的发现及环境演化

  21. High-resolution simulations of the last glacial maximum climate over europe : a solution to discrepancies with Continental palaeoclimatic reconstructions ?

    对欧洲晚冰川极限气候的高分辨率模拟:能解决与大陆古气候重建的偏差吗?

  22. The geological evidence of the global moisture condition changes since the last glacial maximum : the construction of global Lake status data base & the synthesis in the large spatio-temporal scale

    末次盛冰期以来全球湿润状况的地质证据&全球古湖泊数据库及其湖水位变化的大尺度时空分析

  23. Our objective is to examine the shift in the path of the Kuroshio and the interaction be-tween land and sea during the last glacial maximum ( LGM ) .

    目的在确定末次盛冰期时古黑潮流域模式以及海陆气候相互作用。

  24. The 8 m long profile covers the last 30 000 years including the late stage of Marine Oxygen Isotope Stage 3 , the Last Glacial Maximum , the Termination and the Holocene .

    该孔长8m,底部14C年龄为30000aBP,跨越了深海氧同位素3期、末次冰期、冰消期和全新世几个地质历史阶段。

  25. The provenance of the sediment in middle Okinawa Trough during the Last Glacial Maximum is the shelf of the East China Sea . The characteristics of elemental geochemistry ascertain that the sediment was derived from the paleo-Changjiang River .

    末次盛冰期冲绳海槽中部陆源物质来源于东海陆架,元素地球化学特征显示这些沉积物主要来源于古长江的入海物质。

  26. Since the Last Glacial Maximum , the riverbed of the Yangtze River mouth region has evolved from the shape of the deep incised-valley to the filling of the palaeo-valley and to the delta development because of the great change of the sea level .

    末次盛冰期以来,由于海面发生大幅度的变化,长江河口段经历了深切古河谷形成古河谷充填三角洲发育的河床演变过程。

  27. It has been demonstrated that the δ ~ ( 18 ) O in the west Pacific significantly decreased since the last glacial maximum together with , however , a few return events such as the cooling events during the Younger Dryas period of 13.7 ~ 12.2 cal .

    赤道西太平洋海区末次盛冰期以来δ18O值显著降低,但有几次回返事件。

  28. The outflow lake stage , which is characterized by tills , occurred in the late glacial interval of the Last Glacial Maximum , when the watershed of the main ridge zone of the Himalayas shifted northward to the location of present Tangla Mountain .

    外流湖期发育于末次冰期晚冰阶,以冰碛为主要特征,此时喜马拉雅山主脊带分水岭北移至现今荡拉山的位置;

  29. However , the scale of glacial advance during MIS 3 / 4 even exceeded that of the Last Glacial Maximum .

    末次盛冰期的冰川范围十分有限,并且MIS3阶段的冰进规模远远超过了末次盛冰期。