冰期

基本解释 (translations)

iceage

词组短语

ice age

与冰期相关的网络例句 [注：此内容来源于网络，仅供参考]

Of or relating to the fourth glacial stage of the Pleistocene Epoch in North America.

冰期后的与冰期后的时期有关的，或在冰期后的时期里发生的

The principal indicators for recognition of glacial event are presented ,based mainly on various features of the Luoquan Glacial Epoch of Late Sinian , combining with the features of the Nantuo and other glacial epoches .

本文以震旦纪末罗圈冰期的各种特征为基本依据，综合南沱冰期及其它冰期的特点，提出识别冰川事件的主要标志：1。分选性极差的杂砾岩；2。

Based on investigations and studies of modern and ancient glaciers at the Tanggula Mountain pass, coupled with the GPS data and TL, 10B-26Al-21Ne and 14C dating data, Quaternary remnants of glaciation in the study area are discussed in detail. Two glacial epochs (i.e., the late Middle Pleistocene penultimate glacial epoch and the mid-late Late Pleistocene last glacial epoch) arid two Holocene glacial advances (i. e. the Neoglaciation and the Little Ice Age) have been intensively studied.

在对唐古拉山口现代冰川和古冰川考察研究的基础上，结合定位观测资料和TL、10B-26Al-21Ne及14C测年数据，对区内第四纪冰川遗迹进行了深入讨论，划分出二次冰期（即中更新世晚期的倒数第二次冰期、晚更新世中－晚期的末次冰期）和二次全新世冰进。

We suggested that, in the last 130ka, the prominently lake expanding period i.e. the pan-lake period, probably have come into being at MIS5e、MIS5c、MIS5a、 MIS3c、MIS3a, corresponding to high summer solar radiation stages of middle and low latitude in northern Hemisphere, which were in phased with 20ka-cycle. MIS5e was the warmest and wettest stage of the last interglacial, and the other stages were the interstadial of the last interglacial.

对青藏高原及上述诸地区末次间冰期以来气候记录的对比分析揭示：末次间冰期以来，青藏高原湖泊淡化、湖面显著扩涨期，即泛湖期，可能对应于MIS5e、MIS5c、MIS5a、MIS3c、MIS3a，即末次间冰期各暖湿期，末次冰期间冰阶；其分别产生于北半球中、低纬度夏季高太阳辐射阶段，具有准20ka周期演化特征，夏季风降水是造成湖泊扩涨的控制因素。

Theδ〓O fluctuation showed that during the Last Glaciation there existed at least seven warm and five cold climatic fluctuations or events in the east Tibetan plateau, and that during the Last Interglacial Age there existed clearly 5 climatic substages, namely 5a to 5e, among which substage 5e was the warmest climate period, but 5a was an optimum episode of moisture and heat combination.

对末次间冰期及末次冰期气候特征研究表明，青藏高原东部末次间冰期内部存在着5个十分清晰的气候亚期，其中5a、5c、5e三次暖事件以5e温度最高，但水热配置最好的是5a。

The glacial rock surface on the independent hill near Laolinkou Daoban was formed in MIS6. The roche moutonnee in the north of Mountain Tuershang was formed in MIS2. Normally , the distance glacial reached is further and the height of glacial is bigger, the scale of ice age is bigger.

根据三组样品所反映的三次冰期来看，形成于倒数第三次冰期的老终垄的保存，以及形成于倒数第二次冰期的冰川擦痕面的存在，说明最近三次冰期的规模由大到小依次为倒数第三次冰期、倒数第二次冰期和末次冰期。

They have several meters of paleosol developed on the top of overbank silt, suggesting that the abandonment of each terrace due to river incision occurs during the transition from glacial to interglacial climates and there may be a link between the production of terraces and glacial-interglacial climatic cycles. However, it is not every glacial-interglacial transition during the last 1,240ka that terrace can form and preserve.

黄河各阶地河漫滩顶部都有一层古土壤发育表明黄河下切形成阶地发生在古土壤开始发育的冰期向间冰期的过度阶段，但是并非1，240ka以来的每次冰期—间冰期的气候交替都能引起黄河下切形成阶地。

The down core changes of Florisphaera profunda percentage content implied that the thermocline was shallower in glacial periods and deeper in interglacial periods, which might be the direct controlling factors of WPWP productivity changes. It is speculated that the glacial-interglacial fluctuation of the depth of thermocline was induced by the super-ENSO variation.

钙质超微化石下透光带属种Florisphaeva profunda百分含量指示的温跃层深度变化表明冰期温跃层浅、间冰期温跃层加深，这说明类ENSO式变化导致的冰期-间冰期温跃层深度波动可能是MIS7期以来暖池核心区古生产力在冰期高而在间冰期显著降低的直接控制因素。

It is perfectly recorded in these 2 lake cores that the transfer from stage 3 to Last Glacial Maximum and from Last Glacial Maximum to Holocene. The record of pollen in lake core 98-4-A show that there are an abundance of species in Arctic ecosystem, the ecosystem was havocked at Last Glacial Maximum, and is resuming gradually in Holocene.

这两支湖泊岩芯完整地记录了北极巴罗地区从3阶段到盛冰期的转换、从盛冰期到全新世的转换。98-4-B湖泊岩芯的孢粉记录表明，末次盛冰期前北极地区的生态系统物种丰富，末次盛冰期时被严重破坏，全新世时期逐步恢复。

Two major Neoproterozoic glaciations are Marinoan and Sturtian. A number of studies suggested that the Marinoan glaciation terminated about 635 Ma ago, hut the time of its beginning is uncertain.

新元古代末期两次主要的冰期事件是Marinoan冰期和Sturtian冰期，其中Marinoan冰期结束于635Ma；Sturtian冰期可能发生在710~720Ma，已发表的年龄数据限定它在670Ma之前结束。

与冰期相关的网络解释 [注：此内容来源于网络，仅供参考]

great glacial epoch：大冰期

greasy lustre 脂肪光泽 | great glacial epoch 大冰期 | great ice age 大冰期

glacial period：冰期

两个冰期(glacial period)之间的时期,称为间冰期. 间冰期的气候较冰期温暖,因此冰川融化退缩,海面上升. 间冰期的时间也长於冰期,通常说,更新世(pleistocene)有四个冰期和三个间冰期,目前我们的时代为后冰期,若在未来又有一次冰期,则我们这个时代也是个间冰期了

Ice Age：冰期

冰期 (ice age) 具有强烈冰川作用的地史时期. 又称冰川期. 冰期有广义和狭义之分,广义的冰期又称大冰期,狭义的冰期是指比大冰期低一层次的冰期. 大冰期是指地球上气候寒冷,极地冰盖增厚、广布,中、低纬度地区有时也有强烈冰川作用的地质时期.

interglacial epoch：间冰期

它提供相当多种类的金属与非金属矿...时间第四纪大冰期的全球性冰川活动约从距今200万年前开始直到现在,是地质史上距今最近的一次大冰期. 在这次大冰期中,气候变动很大,冰川有多次进退,分别被称为冰期(glacial epoch)和间冰期(interglacial epoch). 第四纪大冰期比以前的冰...

interglacial epoch：冰期

第四纪大冰期的全球性冰川活动约从距今200万年前开始直到现在,是地质史上距今最近的一次大冰期. 在这次大冰期中,气候变动很大,冰川有多次进退,分别被称为冰期(glacial epoch)和间冰期(interglacial epoch).

interglacial phase：间冰期相

间冰期堆积 interglacial deposit | 间冰期相 interglacial phase | 间冰期 interglacial stage

interstadial：次冰期[的]

interstade 次冰期 | interstadial 次冰期[的] | interstadial period 次冰期

Mindel glaciation：民德冰期

民德(冰期) Mindel | 民德冰期 Mindel glaciation | 民德---里斯间冰期 Mindel-Riss interglaciation

Mindel glacial age; Mindel glaciation：民德冰期

民德冰期 Mindel | 民德冰期 Mindel glacial age; Mindel glaciation | 民德、利斯间冰期 Mindel-Riss

Mindel-Riss interglacial：民德-里斯间冰期,明德-里斯冰期

Mindeasing Tonic Pills of Arborvitae Seed ==> 柏子养心丸 | Mindel-Riss interglacial ==> 民德-里斯间冰期,明德-里斯冰期 | mine ==> 矿井,矿山,雷,开采,地雷坑