glacial period

The big glacial period in geological history and it 's composition analysis

地质历史中的大冰期及其成因分析

Dali glacial period in the Northwest Yunnan and rate of crustal deformation in post ~ glacial period

滇西北大理冰期及冰后期地壳变形速率

On basic features of climate and environment in Quaternary glacial period in eastern China

中国东部第四纪冰期气候与环境的基本特征

Evolution of natural environment in China since the last glacial period and its position in the global change

末次冰期以来中国自然环境变迁及其与全球变化的关系

Climate Effect of Dust Aerosol in Southern Chinese Loess Plateau Since the Last Glacial Period

黄土高原南部末次冰期以来沙尘气溶胶的气候效应

A new note on Quaternary glacial period in the Lushan mountain , east China

庐山第四纪冰期研究的新认识

Evidence of fossil Ostracodes for environmental changes of Bohai Sea since late glacial period

渤海晚冰期以来环境变化的化石介形类证据

Two thirds of the continent is covered in ice during glacial period .

该大陆的三分之二地区在冰河时代被冰覆盖著。

Sequence of Quaternary glacial period in Qinghai Xizang Plateau and its significance

青藏高原第四纪冰期序列及其意义

Late glacial period , I assume .

也许是后冰川时期。

Environmental Significance and Characteristics of Grain Size of the Loess in Longxi Basin during the Last Glacial Period

陇西盆地末次冰期黄土粒度特征及其环境意义

Heinrich Events Identified by Gamma Logging Curve During the Last Glacial Period in Qaidam Basin

柴达木盆地应用自然伽玛反演辨认的末次冰期以来的Heinrich事件

Modeling of the tide wave system changes in the marginal seas adjacent to eastern China since the last full glacial period

末次冰期最盛时期以来中国东部边缘海潮波系统演变过程的模拟研究

Dali glacial period in Liaoning Province

辽宁的大理冰期

On the buried Aeolian Loess Strata of the last glacial period in the floor of the East China Sea

东海海底末次冰期埋藏风尘黄土地层初步研究

And was poor during cold and dry glacial period indicated by heavier δ ~ ( 13 ) C.

而冷干的冰期时，植被覆盖减少，δ~（13）C值偏重。

Cathaya argyrophylla is relic plant from the third glacial period , which has great research value .

银杉是第三纪冰川的遗孑植物，具有重大的科研价值。

The MIS 3 is a special period of the last glacial period and similar to the environment of Holocene on some ways .

深海氧同位素第3阶段是末次冰期中的一段特殊时期，与全新世存在一定的相似性。

Distribution and ecology of diatom mat deposits in the West low-latitude Pacific Ocean during the last glacial period

末次冰期低纬度西太平洋硅藻席沉积与生态特征

The current epoch , known as the Holocene , began around 11700 years ago at the end of the last glacial period .

现在这个被称为全新世的时代大约始于11700年前的最后一个冰河时期的末期。

Little is known about climatic conditions in the tropics during the last glacial period and the deglaciation that followed .

人们对最后一次冰期热带的气候条件以及随后发生的冰川消退知之甚少。

The many animals which have remained unchanged since the commencement of glacial period , would have been an incomparably stronger case .

有许多动物，自冰河时代初期以来，迄无改变，这是一个无可比拟的更特殊的例子。

Mount Xishan is the classic area for study of the eolian loess and paleoclimate of the last glacial period in China .

北京西山是中国末次冰期旋回风成黄土与古气候研究的经典地区。

The High Resolution Climate Records from Two Stalagmites in Qixing Cave of Guizhou and the Heinrich Events of the Last Glacial Period

末次冰期贵州七星洞石笋高分辨率气候记录与Heinrich事件

From late Holocene to now , the climate changes to be dry and cold , but its changing scope is smaller than that of last glacial period .

全新世晚期至今，气候向干冷方向转化，但变化幅度远小于末次冰期。

However , the problem is worth further studying that whether there were traces of glaciation during the last glacial period in the past 23 ~ 12 ka .

至于是否存在末次冰期盛冰阶时期的冰川遗迹和冰臼则值得进行进一步研究和讨论。

The loess along south Liaoning seashore derived from Bohai seabed during the last glacial period when sea level was low was transported and deposited by northwest wind in a short distance .

辽南滨海黄土具有沙黄土特征，主要由末次冰期低海面裸露的渤海海底物质经西北风短距离搬运堆积而成；

Stratigraphic record of U_ ( 37 ) ~ K ,δ ~ ( 18 ) O : SST and sea level change in the northern part of South China Sea since the last glacial period

U（37）~K，δ~（18）O沉积地层记录：南海北部末次盛冰期以来SST和海面变化

Then the genetic diversity has decreased when the glacial period came . At the late glacial period about 18000 years ago , the eastern populations started to expand to the center and western China .

之后进入了寒冷的冰川期，遗传多样性降低；到了冰川末期约18000年前，东部种群又开始逐步扩张，并向中西部地区扩散。

Considered of the genetic diversity of the 4 possible wild populations combined with the ecological environment of their habitats , populations WC and TM are regarded as the survival habitats in glacial period .

结合各群体所在地的生态环境综合考虑，认为WC和TM两群体所在地最有可能为野生银杏冰川期避难所。