古新世-始新世,Paleocene-Eocene英语短句,例句大全

古新世-始新世,Paleocene-Eocene
1)Paleocene-Eocene古新世-始新世
2)the Early Tertiary古始新世
3)Eocene Epoch古近纪始新世
1.Zurhen Ul, Qinghai-Tibet Plateau yields Ar Ar ages of (40 91±1 18) Ma, (41 07±0 80) Ma,( 42 00±1 31) Ma and (39 00±2 06) Ma which suggests a large-scale volcanism in the research area in the Middle Eocene Epoch.它们代表了这些火山岩的形成时代 ,表明本区在古近纪始新世中期发生过大规模的火山活
4)Eocene[英]['i:?si:n][美]['i?,sin]始新世
1.On Metasequoia in Eocene Age from Liaoning Province of Northeast China;中国辽宁省始新世水杉的研究
2.Provenance Analysis of Late Cretaceous-Early Eocene Sandstones in the Sangdanlin Area, Southern Tibet;藏南桑单林地区晚白垩世—始新世砂岩物源区分析
3.Quantitative Reconstruction of the Eocene Palaeoclimate in the Fushun Basin,Liaoning Province;辽宁抚顺盆地始新世古气候定量研究

英文短句/例句

1.It intruded Eocene sandstones.它侵入始新世砂岩。
2.small order of primitive ungulates of the Paleocene and Eocene.生活于古新世至始新世的小型原始有蹄动物目。
3.MAMMALS FROM THE MIDDLE EOCENE. KUANCHUANG FORMATION OF XINTAI, SHANDONG山东新泰中始新世化石哺乳类新材料
4.A NEW BRONTOTHERE FROM LATE MIDDLE EOCENE OF QUFU, SHANDONG记山东曲阜中始新世晚期─雷兽新属种
5.Beibu Wan Basin was a lake in the middle Eocence-Lower Oligocene.北部湾盆地在中始新世至早渐新世是一个湖泊。
6.NOTES ON SOME EARLY EOCENE MAMMALIAN FOSSILS OF HENGTUNG,HUNAN湖南衡阳盆地早始新世哺乳动物化石
7.EOCENE PALYNOLOGICAL ASSEMBLAGES AND ENVIRONMENTS IN THE BAISE BASIN OF GUANGXI广西百色盆地始新世孢粉组合与环境
8.Eocene Palynoflora from Changchang Basin,Hainan Island海南岛长昌盆地始新世孢粉植物区系
9.SOME NEW GENERA OF LATE CRETACEOUS TO EOCENE MICROPHYTOPLANKTON FROM WESTERN TARIM BASIN IN SOUTHERN XINJIANG新疆塔里木盆地西部晚白垩世—始新世微体浮游植物的几个新属
10.MIDDLE EOCENE MAMMALS OF JEMINAY, XINJIANG新疆吉木乃地区始新世中期哺乳动物化石
11.SOME EOCENE MAMMALS FROM THE UQBULAK AREA OF THE JUNGGAR BASIN,XINJIANG新疆准噶尔盆地三个泉地区几种始新世哺乳类
12.RECENT PROGRESS ON STUDY OF EOCENE MAMMALS IN YUANQU BASIN垣曲盆地始新世哺乳动物研究的新进展
13.GLOBAL CLIMATE EVENT AT THE EOCENE-OLIGOCENE TRANSITION: FROM GREENHOUSE TO ICEHOUSE始新世—渐新世界线的全球气候事件:从“温室”到“冰室”
14.THE REFLECTIONS OF GLOBAL TECTONICS EVENTS AT THE PALEOCENE EOCENE BOUNDARY IN SEDIMENTOLOGY古新世—始新世界线全球构造事件在沉积学中的反映
15.THE DIVISION OF PALEOCENE AND EOCENE DEPOSITS IN THE NORTHERN JUNGGAR BASIN准噶尔盆地北缘古新世和始新世地层的划分及其时代
16.MINERALOGY IN STRATA AROUND THE BOUNDARY BETWEEN EOCENE AND OLIGOCENE AT SITE 573 IN EAST PACIFIC东太平洋地区573孔始新世末—渐新世初地层矿物学
17.THE CHARACTERISTICS AND REEs GEOCHEMISTRY IN THE STRATA FROM LATE EOCENE TO EARLY OLIGOCENE IN SITE 573, THE EASTERN PACIFIC东太平洋573孔始新世末渐新世初地层特征及稀土元素地球化学
18.LATE EOCENE AND OLIGOCENE CHAROPHYTES FROM THE DONGPU AREA, HENAN AND THEIR PALAEOENVIRONMENTAL SIGNIFICANCE河南东濮地区晚始新世至渐新世轮藻植物群及其古环境探讨

相关短句/例句

the Early Tertiary古始新世
3)Eocene Epoch古近纪始新世
1.Zurhen Ul, Qinghai-Tibet Plateau yields Ar Ar ages of (40 91±1 18) Ma, (41 07±0 80) Ma,( 42 00±1 31) Ma and (39 00±2 06) Ma which suggests a large-scale volcanism in the research area in the Middle Eocene Epoch.它们代表了这些火山岩的形成时代 ,表明本区在古近纪始新世中期发生过大规模的火山活
4)Eocene[英]['i:?si:n][美]['i?,sin]始新世
1.On Metasequoia in Eocene Age from Liaoning Province of Northeast China;中国辽宁省始新世水杉的研究
2.Provenance Analysis of Late Cretaceous-Early Eocene Sandstones in the Sangdanlin Area, Southern Tibet;藏南桑单林地区晚白垩世—始新世砂岩物源区分析
3.Quantitative Reconstruction of the Eocene Palaeoclimate in the Fushun Basin,Liaoning Province;辽宁抚顺盆地始新世古气候定量研究
5)Late Eocene晚始新世
1.They represent the first records of the Pri- mates in Late Eocene of Nei Mongol.记录了内蒙古晚始新世的3种原始灵长类化石(Eosimias sp。
2.All of them represent the first records of their kinds in Late Eocene of Nei Mongol.上述啮齿类的发现也证明呼尔井组的时代为晚始新世。
3.They represent the first cricetids ever found in Late Eocene of Nei Mongol.描述了产自内蒙古晚始新世地层中的3属5种仓鼠化石(Pappocricetodon antiquus,Pap- pocricetodon sp。
6)Middle Eocene中始新世
1.This animal found in Yuanqu Basin not only extends its geographical distribution but also increasesYuanqu Fauna s composition and provides new evidence that Hedi Formation is ofSharamurunian, late Middle Eocene in age.这种化石在垣曲盆地发现，不仅扩大了该动物的地理分布，而且为河堤组的地质时代为沙拉木伦期——中始新世晚期增添了新的证据。
2.Members of the subfamily Ischyromyinae, the most derived of the Paleogene rodent family Ischyromyidae, have previously been reported only from North America,where they are relatively abundant in deposits ranging in age from lare Middle Eocene through Middle Oligocene.特别是由于它比较原始，可能它出现的时代较早，进一步确认长辛店组的时代为中始新世晚期。