pliocene
美 
英
- adj.上新世的；上新统的；第三纪的
- n.上新世；上新统
- 网络之上新世；上新世阶段；第三纪上新世
英汉解释
英英解释
例句
The tiger then began to evolve into a unique species toward the end of the Pliocene epoch, about 3. 2 million years ago.
而320万年前，老虎就以作为上世纪末独一无二的品种进行着演化。
The state of the ice sheets during the Pliocene is not well known, but it is thought that sea level ranged up to 80 feet higher than today.
那时冰川的情况并不清楚，但据说那时的海平面要比现在高80英尺。
Climate models used to predict modern levels of man-made global warming, temperatures in the mid-Pliocene should have been lower.
用来预测现代的人为全球变暖程度的气候模型显示，中新世的气温应该更低。
It is shown that the uplift of the middle Taihang Mountains occurred mainly between the end of Pliocene and Early Pleistocene.
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。
The Yuhuatai Formation is another sand-gravel sequence overlying the Liuhe Formation and its age is late Pliocene .
雨花台组沉积是位于六合组之上的另一套砂砾层，其沉积时代为上新世晚期。
The fast growth of the salt structure took place from the middle-late Pliocene to Quaternary, featuring quick and differentiated growth.
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 Guiwu Formation contains the upper part of the former Xiacaowan Formation and considered to be of Pliocene age.
桂五组则包括原“下草湾组”的上段，时代为上新世。
Molecular phylogenetic studies indicated that genera of Phasianidae originated mainly in Pliocene.
分子进化的研究表明雉科各属的起源主要集中在上新世。
In the Pliocene epoch , 5 . 3 Million years ago , the primates continued to diversify .
在上新纪世纪，5。3百万年前，大主教继续多样化。
The L ate Pliocene-Holocene volcano eruptions were not related with the collision oft he India-Eurasian plates in southwestern China.
上新世晚期—更新世以来的火山活动与中国西南部地区的大陆板块间的碰撞作用没有关系。
So scientists often look to this so-called Pliocene warm period for hints about our future climate.
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。
The first recognisable ancestors of modern humans evolved during the Pliocene epoch.
现代人类第一代可辨认的祖先就是在上新世进化而来。
Pliocene -Holocene Neotectonism has played a key role in formation of Tertiary oil and gas fields in Bohai Sea.
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。
The Wuboer thrust construction started at the Late Pliocene and is active at present.
乌泊尔逆冲推覆构造始于晚上新世，且一直持续活动至今。
The Pliocene ended around three million years ago with the onset of large ice sheets in the Northern Hemisphere.
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 strata of Miocene and Pliocene in the study area deposit in the deepsea plain and toe of slope.
中新世至上新世，研究区发育深海平原和陆坡坡脚沉积。
Hu, C. -H. (1986) Pliocene ostracods from Shoushan, Kaohsiung, southern Taiwan. Petroleum Geology of Taiwan, 22, 103-125.
胡忠恒（1986）台湾南部高雄寿山上新世介形虫化石。台湾石油地质，第22号，第103-125页。
Vegetation succession and climate changing since the Late Pliocene in Tianzhu Region in Beijing
北京天竺晚上新世以来植被演替与气候变迁
Modeling the middle Pliocene climate with a global atmospheric general circulation model
全球大气环流模式用上新世中期气候
Early Pliocene Precession Rhythm of African Monsoon and Mediterranean Sea Surface Productivity
早上新世非洲季风与地中海表层生产力变化的岁差节律
Simulations of warm tropical conditions with application to middle Pliocene atmospheres
带有应用于中上新世大气的温热带条件下的模拟
the newest movable of east-west rupture begins the early Pleistocene and Pliocene;
研究区内东西向断裂最新活动期主要始于早更新世和上新世；
Fan-delta deposits of the pliocene atushi formation in the Southwest Depression, Tarim basin
塔里木西南坳陷上新统阿图什组扇三角洲沉积
Analysis on ore-formation conditions of sandstone-type uranium deposit in Pliocene series, Wulanhua basin, Inner MongoLia
内蒙古乌兰花盆地上新统砂岩型铀矿成矿地质条件分析
Petrogeochemical characteristics of Lower Cretaceous and Pliocene rocks and paleoclimate evolution in Wulanhua region
乌兰花地区下白垩统、上新统岩石地球化学特征及其古气候演变
Magnetostratigraphic Dating on the Pliocene Mammalian Fauna of the Gaotege Section, Central Inner Mongolia
内蒙古高特格含上新世哺乳动物化石地层的磁性年代学研究
The phytolith of Later Pliocene in colorful sand forest of Luliang, Yunnan
云南陆良彩色沙林晚第三纪地层中的植硅石
Magnetostratigraphy of a late Miocene-Pliocene loess-soil sequence in the western Loess Plateau in China
在中国西部黄土高原中新世纪-上新世纪晚期黄土序列的磁层图示法
