pliocene
美 
英
- adj.上新世的；上新統(tǒng)的；第三紀(jì)的
- n.上新世；上新統(tǒng)
- 網(wǎng)絡(luò)之上新世；上新世階段；第三紀(jì)上新世
英漢解釋
英英解釋
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320萬年前，老虎就以作為上世紀(jì)末獨(dú)一無二的品種進(jìn)行著演化。
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.
那時(shí)冰川的情況并不清楚，但據(jù)說那時(shí)的海平面要比現(xiàn)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.
用來預(yù)測現(xiàn)代的人為全球變暖程度的氣候模型顯示，中新世的氣溫應(yīng)該更低。
It is shown that the uplift of the middle Taihang Mountains occurred mainly between the end of Pliocene and Early Pleistocene.
研究同時(shí)表明，太行山中段上新世晚期以來的隆升主要發(fā)生于上新世末到早更新世時(shí)期。
The Yuhuatai Formation is another sand-gravel sequence overlying the Liuhe Formation and its age is late Pliocene .
雨花臺組沉積是位于六合組之上的另一套砂礫層，其沉積時(shí)代為上新世晚期。
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紀(jì)進(jìn)入快速生長期，晚期鹽構(gòu)造生長速率高且差別大。
The Guiwu Formation contains the upper part of the former Xiacaowan Formation and considered to be of Pliocene age.
桂五組則包括原“下草灣組”的上段，時(shí)代為上新世。
Molecular phylogenetic studies indicated that genera of Phasianidae originated mainly in Pliocene.
分子進(jìn)化的研究表明雉科各屬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 .
在上新紀(jì)世紀(jì)，5。3百萬年前，大主教繼續(xù)多樣化。
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—更新世以來的火山活動與中國西南部地區(qū)的大陸板塊間的碰撞作用沒有關(guān)系。
So scientists often look to this so-called Pliocene warm period for hints about our future climate.
因此科學(xué)家們經(jīng)常在所謂上新世暖溫期中尋找有關(guān)未來氣候的線索。
The first recognisable ancestors of modern humans evolved during the Pliocene epoch.
現(xiàn)代人類第一代可辨認(rèn)的祖先就是在上新世進(jìn)化而來。
Pliocene -Holocene Neotectonism has played a key role in formation of Tertiary oil and gas fields in Bohai Sea.
在影響渤海海域上第三系大型油氣田形成的諸多因素中，上新世—全新世的新構(gòu)造運(yùn)動起到了關(guān)鍵作用。
The Wuboer thrust construction started at the Late Pliocene and is active at present.
烏泊爾逆沖推覆構(gòu)造始于晚上新世，且一直持續(xù)活動至今。
The Pliocene ended around three million years ago with the onset of large ice sheets in the Northern Hemisphere.
上新世大約結(jié)束于三百萬年前發(fā)生在北半球大冰原之間的碰撞。
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，研究區(qū)發(fā)育深海平原和陸坡坡腳沉積。
Hu, C. -H. (1986) Pliocene ostracods from Shoushan, Kaohsiung, southern Taiwan. Petroleum Geology of Taiwan, 22, 103-125.
胡忠恒（1986）臺灣南部高雄壽山上新世介形蟲化石。臺灣石油地質(zhì)，第22號，第103-125頁。
Vegetation succession and climate changing since the Late Pliocene in Tianzhu Region in Beijing
北京天竺晚上新世以來植被演替與氣候變遷
Modeling the middle Pliocene climate with a global atmospheric general circulation model
全球大氣環(huán)流模式用上新世中期氣候
Early Pliocene Precession Rhythm of African Monsoon and Mediterranean Sea Surface Productivity
早上新世非洲季風(fēng)與地中海表層生產(chǎn)力變化的歲差節(jié)律
Simulations of warm tropical conditions with application to middle Pliocene atmospheres
帶有應(yīng)用于中上新世大氣的溫?zé)?/c>帶條件下的模擬
the newest movable of east-west rupture begins the early Pleistocene and Pliocene;
研究區(qū)內(nèi)東西向斷裂最新活動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統(tǒng)阿圖什組扇三角洲沉積
Analysis on ore-formation conditions of sandstone-type uranium deposit in Pliocene series, Wulanhua basin, Inner MongoLia
內(nèi)蒙古烏蘭花盆地上新統(tǒng)砂巖型鈾礦成礦地質(zhì)條件分析
Petrogeochemical characteristics of Lower Cretaceous and Pliocene rocks and paleoclimate evolution in Wulanhua region
烏蘭花地區(qū)下白堊統(tǒng)、上新統(tǒng)巖石地球化學(xué)特征及其古氣候演變
Magnetostratigraphic Dating on the Pliocene Mammalian Fauna of the Gaotege Section, Central Inner Mongolia
內(nèi)蒙古高特格含上新世哺乳動物化石地層的磁性年代學(xué)研究
The phytolith of Later Pliocene in colorful sand forest of Luliang, Yunnan
云南陸良彩色沙林晚第三紀(jì)地層中的植硅石
Magnetostratigraphy of a late Miocene-Pliocene loess-soil sequence in the western Loess Plateau in China
在中國西部黃土高原中新世紀(jì)-上新世紀(jì)晚期黃土序列的磁層圖示法
