?Pliocene

Pliocene 發(fā)音

[ 'pla??,sin]

英：　　美：

Pliocene 中文意思翻譯

Pliocene 網(wǎng)絡(luò)釋義

n. 上新世adj. 上新世的

Pliocene 短語(yǔ)詞組

1、Pliocene epoch un. ─── 上新世

Pliocene 相似詞語(yǔ)短語(yǔ)

1、picene ─── n.二萘品苯

2、Pleiocene ─── adj.上新世的

3、Oligocene ─── n.漸漸統(tǒng)；漸新世；adj.漸漸統(tǒng)的；漸新世的

4、paleocene ─── n.古新世

5、pulicene ─── 清潔

6、Miocene ─── adj.第三紀(jì)中新世的；n.第三紀(jì)中新世；中新世沉積巖

7、Eocene ─── adj.始新世的；n.始新世

8、Pleistocene ─── adj.更新世的；n.更新世；更新世巖

9、Pliocene ─── adj.上新世的；n.上新世，上新世巖

Pliocene 常見例句（雙語(yǔ)使用場(chǎng)景）

1、some gas pools in the Pliocene and Pleistocene of the Gulf Coast seem to be of this relatively immature thermal derivation ─── 墨西哥灣岸盆地某些漸新統(tǒng)和更新統(tǒng)氣藏可能就屬于這類相對(duì)低成熟的熱成因氣。

2、In addition, we obtained one OSL sample in the fluvial facies, and this fluvial facies is unconformable on the Pliocene Series. ─── 另外在一個(gè)觀察點(diǎn)的不整合于上新統(tǒng)之上的河流相中采取了一個(gè)OSL樣品。

3、EVOLUTIONARY CHARACTERISTICS OF SOLUBLE ORGANIC MATTER IN QUARTERMARY TO PLIOCENE OF THE TSADAM BASIN ─── 柴達(dá)木盆地第四系至上新統(tǒng)可溶有機(jī)質(zhì)的演化特征

4、Rock type classification of Pliocene Epoch lignite in Jinsuo, Yunnan ─── 云南金所上新世軟褐煤的巖石類型分類

5、A type of fan-delta that an alluvial fan progrades into a lake is found in the pliocene Atushi Formation in the Southwest Depression,Tarim Basin. ─── 塔里木盆地西南坳陷上新統(tǒng)阿圖什組中發(fā)育一套沖積扇進(jìn)積到內(nèi)陸湖泊中而形成的扇三角洲沉積體。

6、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(cè)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。

7、Late Pliocene ─── 晚上新世

8、SPATIAL AND TEMPORAL VARIATIONS OF NORTHEAST ATLANTIC CALCAREOUS NANNOFOSSIL ASSEMBLAGE SINCE PLIOCENE ─── 上新世以來東北北大西洋鈣質(zhì)超微化石組合的演變

9、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。

10、any of various extinct elephantlike mammals of the genus Dinotherium that existed during the Miocene,Pliocene,and Pleistocene epochs ─── 恐獸，一種具有明顯類似象的哺乳類動(dòng)物恐獸，存在于中新世、上新世和更新世時(shí)代

11、EVOLUTION OF SEDIMENTARY ENVIRONMENTOF R_1 CORE FROM THE BEIBU GULFSINCE THE PLIOCENE ─── 北部灣R_1鉆孔巖心上新世以來的沉積環(huán)境演變史研究

12、Keywords Yuanmou;Taigu;Fossil wood;Late Pliocene;Palaeovegetation;Palaeoenvironment;Palaeoclimate; ─── 元謀;太谷;化石木;晚上新世;古植被;古環(huán)境;古氣候;

13、The development of the Balouhe Formation discovered at first time in Zibo area,Shandong Province filled the stratum gap of Pliocene system. ─── 上新世巴漏河組在淄博地區(qū)的發(fā)現(xiàn)填補(bǔ)了該地區(qū)上新統(tǒng)的空白。

14、Its geological time, ignored for the early Pliocene, about ape-man Lam and Shaanxi considerable time. ─── 其地質(zhì)時(shí)代、為中理會(huì)新世早期，約與陜西藍(lán)田猿人時(shí)代相當(dāng)。

15、The cover rocks are marine mudstone from Pliocene to Quaternary. ─── 儲(chǔ)層發(fā)育有砂巖、灰?guī)r（礁灰?guī)r）、基巖等。

16、Chang, Stanley(1964) Regional stratigraphic study of the lower Pliocene and upper Miocene formations in the Chiayi and Hsinying area, Taiwan. Petroleum Geology of Taiwan, 3, 1-20. ─── 張錫齡(1964)嘉義及新營(yíng)區(qū)下部上新世及上部中新世地層之區(qū)域性研究。臺(tái)灣石油地質(zhì)，第3號(hào)，第1-20頁(yè)。

17、Keywords fruits and seeds,Ruppia,Miocene,Pliocene,paleovegetation,paleoenvironment,paleoclimate,Yunnan,Shanxi; ─── 果實(shí)和種子;中新世;上新世;古植被;古環(huán)境;古氣候;川蔓藻屬;云南;山西;

18、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(zhǎng)期，晚期鹽構(gòu)造生長(zhǎng)速率高且差別大。

19、extinct primates; lower Pliocene. ─── 上新世后期已滅絕的靈長(zhǎng)類。

20、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

21、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。

22、According to the unearthed fossils, the giant panda appeared primarily in the later stage of Pliocene Epoch in the Tertiary Period. ─── 從出土的大熊貓化石看 ,大熊貓最早產(chǎn)生于地質(zhì)時(shí)代第三紀(jì)的上新世后期 .

23、PLIOCENE QUATERNARY FAULTING PATTERN AND LEFT SLIP PROPAGATION TECTONICS IN NORTH CHINA ─── 華北地區(qū)上新世至第四紀(jì)斷裂作用型式與左旋擴(kuò)展

24、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

25、Pliocene epoch series ─── 上新世(統(tǒng))

26、LATE PLIOCENE CHANGES OF UPPER OCEAN STRUCTURE IN THE SOUTHERN SOUTH CHINA SEA ─── 南沙海區(qū)晚上新世海水上層結(jié)構(gòu)變化

27、The strata of Miocene and Pliocene in the study area deposit in the deepsea plain and toe of slope. ─── 摘要中新世至上新世，研究區(qū)發(fā)育深海平原和陸坡坡腳沉積。

28、The Yuhuatai Formation is another sand-gravel sequence overlying the Liuhe Formation and its age is late Pliocene . ─── 雨花臺(tái)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。

29、the Pliocene ─── 上新世,上新統(tǒng)

30、The Hohhot-Baotou basin was developed on the basis of Paleocene sedimentary basin, and in Pliocene large scale subsidence commenced which built the fundation of huge sedimentary strata. ─── 呼--包盆地是在古近紀(jì)沉降盆地的基礎(chǔ)上發(fā)育起來的，從上新世開始發(fā)生大規(guī)模劇烈沉降，從而奠定了現(xiàn)代巨厚層現(xiàn)代堆積層的基礎(chǔ)。

31、Sedimentary Records and Asian Monsoon in Ninetyeast Ridge of Bay of Bengal since Pliocene Time ─── 孟加拉灣東經(jīng)90°海嶺中上新世以來沉積記錄及亞洲季風(fēng)

32、The oil source of oilsand in northern Kashi sag came from Jurassic hydrocarbon source whose reservoir-forming stage might be from Miocene to Pliocene. ─── 喀什凹陷北部油砂的油源來自于侏羅系烴源巖，成藏期為中新世至上新世。

33、The Pliocene sediments are characterized by larger variations of Ce anomaly and more significant Eu depletion than the Quaternary sediments. ─── 巖芯中上新統(tǒng)沉積物中Ce異常變化大,而Eu虧損相對(duì)第四系沉積物更顯著。

34、Pliocene era oils ─── 上新世石油

35、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

36、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。

37、PLIOCENE ENVIRONMENT OF HIPPARION FAUNA OF MIDDLE HIMALAYA RANGE ─── 喜馬拉雅山中段上新世三趾馬動(dòng)物群生活環(huán)境的探討

38、Different stress mechanisms and stress strengths resulted in the structural deformation characteristics of different segments in E-W direction since Pliocene. ─── 上新世以來盆地構(gòu)造變形的東西分段是由不同的應(yīng)力機(jī)制和應(yīng)力強(qiáng)度引起。

39、Pliocene horse approaching donkeys in size. ─── 上新世的馬，大約如猴子大小。

40、PLIOCENE RHODODENDRON AND PINUS FOSSIL WOODS OF YUNNAN PROVINCE AND PALAEOCLIMATE ─── 云南上新世杜鵑屬和松屬化石木研究及其古氣候意義

41、The Eocene to Pliocene was generally wetter than today but increasingseasonality in rainfall led to the development of scleromorphy and xerophyfism fromabout the Miocene onwards. ─── 從始新世到上新世，澳大利亞的氣候總體上要比現(xiàn)在濕潤(rùn)，但降水量季節(jié)性變化的增強(qiáng)推動(dòng)了中新世以后硬葉植物和旱生植物的發(fā)展。

42、The Pliocene Epoch or its system of deposits. ─── 上新世，上新世巖上新世或它的沉淀系統(tǒng)

43、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)釒l件下的模擬

44、Ding Zhongli,Sun Jimin,Zhu Rixiang,et al.Eolian origin of the red clay deposits in the Loess Plateau and implications for Pliocene climatic changes[J].Quaternary Sciences,1997,17(2):147-157. ─── [15]丁仲禮,孫繼敏,朱日祥,等.黃土高原紅粘土成因及上新世北方干旱化問題[J].第四紀(jì)研究,1997,17(2):147-157.

45、A STUDY OF DISPERSED CUTICLES IN THE MANGBANG FOMATION (PLIOCENE) OF TENGCHONG,WESTERN YUNNAN ─── 云南騰沖上新統(tǒng)芒棒組植物分散角質(zhì)層研究

46、Late Miocene-Early Pliocene ─── 晚中新世-早上新世

47、Chang, Stanley(1963) Regional stratigraphic study of Pleistocene and upper Pliocene formations in Chiayi and Hsinying area, Taiwan. Petroleum Geology of Taiwan, 2, 65-86. ─── 張錫齡(1963)嘉義及新營(yíng)區(qū)更新世及上部上新世地層之區(qū)域性研究。臺(tái)灣石油地質(zhì)，第2號(hào)，第65-86頁(yè)。臺(tái)灣地質(zhì)知識(shí)服務(wù)網(wǎng)

48、the Pliocene is piedmont diluvial conglomerates with mudstones; ─── 上新統(tǒng)為山麓洪積相礫巖夾泥巖;

49、pliocene epoch ─── 上新世

50、Typical Convolute Bedding in Pliocene,Jilantai,Nei Mongol ─── 吉蘭泰上新統(tǒng)中的典型旋卷層理

51、Tthe early Pliocene had a weakened atmospheric circulation, and therefore, reduced vertical wind shear, which is favorable for tropical cyclone growth. ─── 上新世早期的大氣環(huán)流被減弱，因此垂直風(fēng)切變減小，助長(zhǎng)了熱帶氣旋的發(fā)展。

52、Any of various extinct elephantlike mammals of the genus Dinotherium that existed during the Miocene, Pliocene, and Pleistocene epochs. ─── 恐獸一種具有明顯類似象的哺乳類動(dòng)物恐獸，存在于中新世、上新世和更新世時(shí)代

53、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。

54、Keywords Pliocene;Cyprideis;Upper Youshashan formation;bio-explosion;Ostracoda;Qaidam basin ; ─── 柴達(dá)木盆地;上新統(tǒng);正星介;上油砂山組;生物爆發(fā);介形類;

55、Pliocene Wood Flora from Yuanmou of Yunnan and Taigu of Shanxi, China ─── 云南元謀和山西太谷上新世木化石群研究

56、PLIOCENE MAMMALIAN FAUNA OF GAOTEGE IN NEI MONGOL (INNER MONGOLIA), CHINA ─── 內(nèi)蒙古高特格上新世哺乳動(dòng)物群(英文)

57、A NEW GENUS OF PLIOHYRACINAE (HYRACOIDEA, MAMMALIA) FROM THE LATE PLIOCENE OF DEGE, SICHUAN, CHINA ─── 四川德格上新蹄兔亞科(Pliohyracinae)一新屬

58、Isn't the mastodon from the Pliocene Epoch? ─── 乳齒象不是上新世的嗎?

59、The Blancan extends back into the Pliocene. ─── 勃朗階延伸回上新世。

60、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

61、Keywords paleochannel;sandstone type uranium deposit;ore formation conditions;Pliocene;Wulanhua basin; ─── 古河道;砂巖型鈾礦;成礦條件;上新統(tǒng);烏蘭花盆地;

62、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。

63、North American cat of the Miocene and Pliocene; much earlier and less specialized than members of the genus Smiledon ─── 中新世和上新世生活在美洲的貓科動(dòng)物；對(duì)其研究也少

64、The variation of the sandstone and conglomerate content in the Miocene to Pliocene regional cap rocks governed the types of the oil reservoirs and their oil contents. ─── 中、上新統(tǒng)區(qū)域蓋層中砂、礫巖含量的變化,控制濟(jì)陽(yáng)坳陷南、北方向上第三系地層油藏類型及其含油性的變化。

65、Steroids from Pliocene Fossil Pinus armandii ─── 上新世華山松化石中的甾體化合物

66、Aim To explore the shallow gas about pleistocene and pliocene strata in Huhe Depression and research, the gas genetic type and accumulation geological faetors. ─── 摘要目的探究呼和拗陷第四系更新統(tǒng)、第三系上新統(tǒng)淺層氣的成氣原因，查明該區(qū)成藏地質(zhì)因素。

67、Trap character is not quite obvious in the Miocene, relatively larger in the Pliocene and weakenin the Pleistocene. ─── 中新世圈閉特征并不十分明顯，上新世形成的較大面積的構(gòu)造圈閉，更新世圈閉特征減弱。

68、Pliocene (series) ─── 上新統(tǒng)

69、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。

70、Pliocene Period ─── 上新世時(shí)期

71、Studies on Gyirong Basin Pliocene sediments showed that the nest composition of the sediments were smectite, kaolinite, chlorite, illite, sanidine, quartz, calcite and less gypsum. ─── 對(duì)吉隆盆地中上新世沉積物的研究表明，沉積物的礦物成分主要由黏土礦物伊利石、高嶺石、綠泥石、蒙脫石以及長(zhǎng)石、石英、方解石及少量的石膏等組成。

72、Those correspond to Quaternary, Pliocene, Upper Miocene, Lower Miocene and Eocene respectively. ─── 分別為第四系、上新統(tǒng)、中新統(tǒng)上段、中新統(tǒng)下段及始新統(tǒng)。

73、North American cat of the Miocene and Pliocene; much earlier and less specialized than members of the genus Smiledon. ─── 中新世和上新世生活在美洲的貓科動(dòng)物；對(duì)其研究也少。

74、VARIATIONS IN UPPER OCEAN STRUCTURE IN THE SOUTH CHINA SEA AND THE EVOLUTION OF THE EAST ASIAN MONSOONS SINCE LATE PLIOCENE ─── 晚上新世以來南海北部上部水體結(jié)構(gòu)變化及東亞季風(fēng)演化

75、The results showed that the sandstone-type Uranium mineralization ages were 82.4 Ma, 60 Ma, 11.4 Ma, 7.1 Ma and 3.5 Ma have been obtained. The main mineralized stage is Miocene Epoch and Pliocene Epoch of Neogene Period. ─── 對(duì)伊犁盆地砂巖型鈾礦床及其蝕源區(qū)的初步研究表明 ,該區(qū)砂巖型鈾礦具有期成礦作用的特點(diǎn) ,成礦年齡有 82Ma、6 0Ma、11 4Ma、7 1Ma和 3 5Ma。

76、LATE PLIOCENE VEGETATION AND CLIMATE OF YANGYI REGION, YUNNAN OF CHINA, RECONSTRUCTED FROM PALYNOLOGICAL DATA. ─── 摘要：云南羊邑晚上新世孢粉植物群含52個(gè)孢粉類型，其中被子植物占61.5%，裸子植物占9.6%，蕨類植物占25.0%，藻類植物占3.9%。

77、Sequence IV is Pliocene sea-onshore transition grayer, grayish gritstone, siltstone and mudstone and becomes thicker sea facies toward trough. ─── 層序IV，為上新統(tǒng)海陸過渡相的灰白、淺灰色砂礫巖、粉砂巖、泥巖，往沖繩海槽方向增厚，變?yōu)楹Ｏ唷?/p>

78、pliocene pleistocene boundary ─── 上新世更新世邊界

79、Fuh, S.-C.Liu, C.-S. and Wu, M.-S.(1997)Migration of canyon systems from pliocene to pleistocene in area between Hsyning structure and Kaoping slope and its application for hydrocarbon exploration. ─── 傅式齊、劉家瑄、吳明賢(1997)新營(yíng)構(gòu)造至高屏斜坡間上新世至更新世之海底峽谷系統(tǒng)遷移及其應(yīng)用于油氣探勘。

80、On the influence of global change of Cenozoic climate and uplift of Himalayas, the area began to present a distinct seasonal climate on the basis of previous warmth and humidity in Pliocene. ─── 受新生代全球氣候變冷和喜馬拉雅運(yùn)動(dòng)的影響，該盆地一方面受印度洋季風(fēng)的影響增強(qiáng)，干濕季節(jié)交替明顯；另一方面受地形地貌影響，沿襲了溫暖濕潤(rùn)的氣候條件。

81、LATE PLIOCENE ENHANCED EAST ASIAN WINTER MONSOON: EVIDENCE OF ISOTOPE AND FORAMINIFERS FROM THE NORTHERN SOUTH CHINA SEA ─── 南海北部上新世晚期東亞冬季風(fēng)增強(qiáng)的同位素和有孔蟲證據(jù)

82、GEOCHEMICAL CHARACTERISTICS OF THE MIOCENE EOLIAN DEPOSITS AND COMPARISON WITH THE PLIOCENE AND QUATERNARY EOLIAN DEPOSITS ─── 中新世風(fēng)塵堆積的地球化學(xué)特征及其與上新世和第四紀(jì)風(fēng)塵堆積的比較

83、Fruits and Seeds from Yunnan in the Age of Miocene and from Shanxi in the Age of Pliocene ─── 云南中新世和山西上新世果實(shí)和種子的研究

84、RESEARCH OF PLIOCENE FLORA AND PALEOENVIRONMENT OF YUSHE BASIN ON SHANXI PLATEAU, CHINA ─── 山西榆社盆地上新世植物群及其環(huán)境意義

85、PLIOCENE COOLING BEFORE THE ICE AGES IN NORTH CHINA ─── 中國(guó)北方上新世降溫事件及其對(duì)溫度緯度梯度變化的影響

86、Post-rifting mainly occurred in Miocene and Pliocene and Quaternary, and formed Guantao，Minghuazhan and Pingyuan Formations. ─── 中南區(qū)斷陷走向呈近東西向、北東向和北西向，斷陷都是北斷南超的半地塹;

87、Doubt about the age of the Pliocene basalts" in Northeast China ─── 對(duì)東北地區(qū)“上新統(tǒng)玄武巖”時(shí)代的質(zhì)疑

88、All the fault-folding tectonic zones at the basins northern margin area are basically fixed by one most intensive structural movement at the end of Pliocene. ─── 上新世末的構(gòu)造運(yùn)動(dòng)是一次最強(qiáng)烈的構(gòu)造運(yùn)動(dòng),使柴北緣地區(qū)各斷褶構(gòu)造帶基本定型。

89、From boundary to centre of the basin,the reservoir beds for exploring for gas are Oligocene,Miocene,Pliocene and Quaternary and the lithology changes from coarseness to fineness. ─── 從盆地邊緣到中心，有勘探意義的儲(chǔ)層依次有漸新統(tǒng)、中新統(tǒng)、上新統(tǒng)和第四系，巖性由粗變細(xì)。