上新世早期的大气环流被减弱，因此垂直风切变减小，助长了热带气旋的发展。
Tthe early Pliocene had a weakened atmospheric circulation, and therefore, reduced vertical wind shear, which is favorable for tropical cyclone growth.
勃朗阶延伸回上新世。
上新世出现断陷，中更新世成湖。
Fault depression took place in Pliocene and the Qinghai Lake formed in Middle Pleistocene.
结合所产化石，其时代为中-上新世。
They are in Miocene Pliocene ages according to the fossils in them.
乳齿象不是上新世的吗？
样品的地层年代介于渐新世和上新世之间。
The samples are from Oligocene, Miocene and Pliocene strata.
上新世和第四纪主要为浅海陆架及半深海充填沉积。
There were mainly neritic shelf and bathyal filling sedimentation in the Pliocene and Quaternary.
上新世晚期，早更新世初期，第二排褶皱开始形成。
The second fold developed between late the Miocene and the initial stage of Early Pleistocene.
上新世-第四纪区域沉降阶段，东西向断层再次活动。
Regional subsidence stage from Pliocene to Quaternary, the EW trending reactivated.
因此，含高山栎岩系的地质时代不会早于上新世中晚期。
The geological age of the present sandstone series is not earlier than the middle-late Pliocene.
上新世大约结束于三百万年前发生在北半球大冰原之间的碰撞。
The Pliocene ended around three million years ago with the onset of large ice sheets in the Northern Hemisphere.
它们现在的构造格局基本上是在晚上新世或早更新世奠定的。
Their tectonic framework was basically underlain in early Pleistocene or late Pliocene.
上新世巴漏河组在淄博地区的发现填补了该地区上新统的空白。
The development of the Balouhe Formation discovered at first time in Zibo area, Shandong Province filled the stratum gap of Pliocene system.
因此科学家们经常在所谓上新世暖温期中寻找有关未来气候的线索。
So scientists often look to this so-called Pliocene warm period for hints about our future climate.
从地层层序和植物群的特点上看，该煤组的地质时代为上新世晚期。
Judging from the stratigraphical sequence and the characteristics of this flora, the geological age of the said coal series is late Pliocene.
该地区分布着两百余座大大小小的火山，形成于中新世、上新世和更新世。
There are more than 200 volcanic hills, mainly occurring in the Miocene, Pliocene and Pleistocene in the region.
上新世中晚期一第四纪进入快速生长期，晚期盐构造生长速率高且差别大。
The fast growth of the salt structure took place from the middle-late Pliocene to Quaternary, featuring quick and differentiated growth.
最晚的化石记录分别发现于北美的中中新世、欧洲的上新世和亚洲的更新世。
Youngest occurrences were found from the Middle Miocene of North America, the Pliocene of Europe, and the Pleistocene of Asia.
结合同位素地质年龄，区域对比分析，确认昔格达组属上新世至早更新世沉积。
Isotopic dating and regional stratigraphic correlation indicate that the Xigeda Formation is Pliocene-Early Pleistocene sediment.
科学家们回溯至三百万年前的上新世，获得了这个证据。当时全球气温比现在高3至5摄氏度。
The evidence was obtained by scientists looking back three million years to the Pliocene epoch, when global temperatures were 5.4f (3c) to 9f (5c) higher than they are today.
本文研究了云南保山地区上新世羊邑组和芒棒组的四种被子植物化石的表皮微细构造。
The cuticular microstructures of four angiosperm fossil plants from the Pliocene Mangbang Formation and the Yangyi Formation in Baoshan, Yunnan Province were studied in this paper.
研究同时表明，太行山中段上新世晚期以来的隆升主要发生于上新世末到早更新世时期。
It is shown that the uplift of the middle Taihang Mountains occurred mainly between the end of Pliocene and Early Pleistocene.
通过共和盆地西北部晚新生代地层的野外地质调查，发现上新世地层中存在一期角度不整合面。
An angular unconformity within the Pliocene stratum was found during field exploration in northwestern part of the Gonghe Basin.
冈底斯西段赛利普一带分布有大面积的钾质火山岩，以前曾被划归上新世一早更新世赛利普群。
Large area of potassic volcanic rocks distributed over the Sailipu area of West Gangdis were originally assigned to the Sailipu Group and the age was Pliocene-Early Pleistocene.
层序IV，在陆坡和岛弧地区都有分布，但是在海槽盆地内部区域缺失该层序，为上新世沉积物。
We found that sequence IV, which is Pliocene sediments, only exists in the slope and island arc slope and not distributes in the trough basin.
在影响渤海海域上第三系大型油气田形成的诸多因素中，上新世—全新世的新构造运动起到了关键作用。
Pliocene-Holocene Neotectonism has played a key role in formation of Tertiary oil and gas fields in Bohai Sea.
来自日本札幌北海道大学的地球化学家渡边刚和他的同事们在菲律宾的珊瑚中找到了上新世中叶的气候线索。
Geochemist Tsuyoshi Watanabe of Hokkaido University in Sapporo, Japan, and his colleagues hunted for climate clues in corals that grew in the Philippines during the mid-Pliocene.
为了研究上新世的飓风活动情况，研究人员依靠的就代理海洋温度，这个温度是基于洋底岩芯里几种化学示踪剂变化引起的。
To investigate the hurricane activity of the Pliocene, the researchers relied on proxy ocean temperatures based on variations in several chemical tracers in drill cores of the ocean floor.
结果表明， 札 达地区上新世—早更新世气候经历了从湿热—温暖潮湿—偏冷潮湿—寒冷干旱的变化，以及植被从森林—灌木—草原的逐渐演化。
They think that the climate change from wet-hot, warm-wet, little cold-wet, to cold-drought, and the vegetational evolution from forest, bush, to grassland in Zhada area.
结果表明， 札 达地区上新世—早更新世气候经历了从湿热—温暖潮湿—偏冷潮湿—寒冷干旱的变化，以及植被从森林—灌木—草原的逐渐演化。
They think that the climate change from wet-hot, warm-wet, little cold-wet, to cold-drought, and the vegetational evolution from forest, bush, to grassland in Zhada area.
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