On the basis of analyzing regional structure and evolution characteristics, It is considered that undergoing 3 evolutions of Eocene-Oligocene, Miocene and Pliocene exploration, Burma central basin Formed in Tertiary and can be divided into 2 secondary grade structural units, i. e. western deep depression and eastern shallow depression, and 11 third grade structural units, such as Irrawaddy sag, Prome sag, Salin sag, Chindwin sag, Hukawng sag, Putao sag, Shwebo sag, Inlelake sag, Salween sag, Sittang sag and Pegu upwarping.
基於对区域构造特徵和演化的分析，认为缅甸中央盆地形成於第三纪，经历了始新世－渐新世、中新世和上新世三期构造演化，可划分为西部深坳区和东部浅坳区2个二级构造单元及Irrawaddy凹陷、Prome凹陷、Salin凹陷、Chindwin凹陷、Hukawng凹陷、Putao凹陷、Shwebo凹陷、Inlelake凹陷、Salween凹陷、Sittang凹陷、Pegu凸起等11个三级构造单元。
The Cenozoic heat flow history of the deep water area of the northern margin of South China Seais estimated through non? instantaneous, non? homogeneous, multi? episode and pure shear model. It shows that the deep water area of the northern margin of SCS has experienced multi? episodes of heating event since Eocene time.
在构造沉降史恢复的基础上确定拉张期次，再采用非瞬时非均匀多期拉张纯剪切模型恢复南海北部深水区新生代热流史，结果表明：始新世以来，南海北部深水区存在多期热流升高的加热事件。
All above significant changes imply that the Tethys-Himalayanarea was affected by the Paleocene/Eocene Thermal Maximum.
西藏南部受全球地质事件的影响，在古新世与始新世界线时期出现明显的气候变化。
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。
I am on an Oligocene beach, an Eocene beach, a Cretaceous beach -- the scene is the same.
我正在渐新统的海滩上，或在始新世的海滩上，或在白垩纪的海滩上——场景不变。
However, there are not only a lot of sporo-pollen assemblages from Eocene to Oligocene but also much more ichthyolite from Oligocene to Miocene.
然而，这套地层中存在大量始新世－渐新世的孢粉组合，同时赋存有相当数量的时代为渐新世－中新世的鱼化石。
Artiodactyla generally divided into:(1) Ancient cloven-hoofed also known as sub-orders of ancient teeth, including the Eocene and Oligocene Some of the early cloven-hoofed, they already have two of the talus trochlear surface.
偶蹄目一般分为：（1）古偶蹄类或称古齿亚目，包括始新世和渐新世的一些早期偶蹄类，它们的距骨已具有两个滑车面。
These stages can be generalized into four cycles: 1 lower Cretaceous to lower Eocene; 2 middle Eocene to Oligocene; 3 Oligocene to Neocene; 4 Quaternary.
从而可以划分出四个构造旋回：1早白垩世—早始新世；2中始新世—渐新世；3渐新世—晚第三纪；4第四纪。
The evolution process under the control of the multigeodynamic force system (including the boundary forces of Eurasia-Pacific-Indian three massive plates around Nansha block, effects of the deep mantle, relative soft layer-sliding planes within Nansha lithosphere block and the earth's rotational inertial force) can be briefly divided four stages: the late Cretaceous to the early Eocene stage of uprilfing-erosion and shear-extension caused by the oceanwards-eastwards withdrew of Pacific subduction zone and the delamination of proto-subducted slab after the stage of pre-Cretaceous pre-rifting active continentoceanic plate margin. In this stage, the Nansha transcrustal layering-block started to move southeastwards on the Nansha transcrustal layer-sliding plane, meanwhile, the Andu-Bisheng and Liyue-Banyue basement layering-block slid on their upper-crust layer-sliding planes, and Xibu accretion zone was formed. Successively, it entered the stage of the mid-Eocene to early Oligocene, when NW-SE sea-floor spreading occurred in the southwest subbasin owing to the slip-line field initiated by the collision between the Indian and Eurasian plates, Zengmu foreland-basin started to develop in the same time. And in the stage of late Oligocene to early Miocene, near NS simple-shear extension and sea-floor spreading in the central subbasin of eastern South China Sea resulted from the south-southeastwards drawing-force of the mantle-flow. The crustal layering-blocks and the Miri accretion zone formed also in this stage.
南沙岩石圈新生代微板块及板内层块构造的动力演化过程，在多元动力等因素(如块体之外的欧-太-印三大板块运动边界力和地幔深部活动因素、块体内部软弱层滑面以及地球自转变化)控制下，大致经历了4个阶段的演化：从前晚白垩世的裂前活动陆-洋板块边缘阶段因太平洋俯冲带向东跃迁、原向NNW俯冲消亡的板片的拆沉、幔隆而进入晚白垩世-早始新世的隆升剥蚀、剪切伸展演化阶段，南沙超壳层块顺超壳层滑面祥东南运移、安渡-毕生与礼乐-半月基底层块沿上壳层滑面拆离，西布增生带形成；继而先后在中始新世-早渐新世期间受印-欧板块碰撞滑线场、地球自转加速影响出现西南海盆NW-SE向海底扩张和曾母前陆盆地的发育，和晚渐新世-早中新世期间南—东南向地幔流牵引造成的中央次海盆近NS向单剪伸展与海底扩张、壳体层块向南差异滑移、米里增生带形成；中中新世以来，印度-澳洲板块快速向北俯冲，构成今日南海格局。
The first rapid subsiding was a result of the combination of extension of Eastern Asia continental margin and the sinistral strikeslip of Red River Fault in Eocene; the second one was related with the seafloor spreading of the South China Sea and sinistral strike. slip of RRF in Oligocene to early Miocene; the third one is mainly controlled by the dextral strike-slip of RRF since 10～5 Ma; the weak subsiding process was coeval with the weakly strike-slipping period of RRF within mid-late Miocene time and a response to the cease of the seafloor spreading of SCS.
第一期快速沉降过程受东亚陆缘扩张和红河断裂左旋走滑共同影响，第二期快速沉降受南海海底扩张和红河断裂左旋走滑联合作用，第三期快速沉降主要受红河断裂右旋走滑控制，缓慢沉降过程与南海海底扩张停止以及红河断裂构造活动处于宁静阶段相耦合。
The Leaf Margin Analysis method was used here to reconstruct Mean Annual Temperature of six Chinese Eocene floras.
文中采用叶缘分析法首次定量重建中国始新世6个植物群的古年均温。
Numerical modeling on the case history reveals that the heat flow progressively decreased from approximately 103-110mW/m〓 in Eocene epoch to nearly 64mW/m〓 in nowdays, which is consistent with the tectonic evolution and magmatic activity of this area got from other data.
以乌参1井、叶2井、叶12井和枣42井为例，以磷灰石裂变径迹(17个样品)为地温计，研究了渤海湾盆地黄骅坳陷南区的构造热历史，数值模拟得乌参1井、叶12井和枣42井在早第三纪末东营组及沙河街组的剥蚀量分别为520m、150m和1600m，揭示的热流从始新世到今由高(103-110mW/m〓)到低(64mw/m〓)的演化规律同此区的构造及岩浆活动规律一致，用乌参1井的R〓数据进行的热史模拟支持了此结论。
We studied a maxillary fragment of tarsier and revealed that tarsiers had already achieved gigantic orbits and bell-shaped palate by the time of middle Eocene.
对于眼镜猴上颌骨片断的研究表明，中始新世的眼镜猴已经具有了如同现生眼镜猴一样的钟形腭和明显增大的眼眶。
The Paleocene-Eocene thermal maximum has been attributed to a sudden release of carbon dioxide and/or methane.
研究人员提出，大约5500万年前在格陵兰岛与欧洲附近发生的一次剧烈的火山爆发，也许触发了古新纪—始新世极热时期。
Nanxiong Basin, brought together a variety of reptiles, in the rivers and lakes along the Strip, to survive, surrounded by mountains processes, a large number of weathered debris deposited by rivers into the basin down the number of dead dinosaur remains or has been swallowed by floods and buried in the dinosaur dinosaur eggs in the soil and remain in the river and lake sediment layer of dinosaur footprints, etc., along with sediments were deeply buried in the ground, after a long process to become a variety of petrochemical fossil, such as dinosaur bones, dinosaur eggs and remains fossils; the late Cretaceous period, subject to the final phase of the impact of Yanshan movement, Nanxiong basin fault activity occurred weak and short-term uplift, Nanxiong Group strata subjected to a period of erosion; to the mid-Cenozoic Paleocene, again under the Nanxiong Basin Shen, their acceptance of the Early Tertiary Zhai Qun Luo Buddha-phase accumulation of lacustrine and alluvial; the early Eocene, uplift of the basin and caused another short-lived hiatus, the latter sinking are also trained in Danxia pluvial phase and rivers and lakes phase accumulation; the late Oligocene, by the Himalayan movement affected the whole basin and the northern part of Guangdong, as elsewhere, the general uplift, accompanied by lifting ramp fault activity, erosion of the basin into areas, southern margin of the basin due to uplift of the higher, first of all eroded overlying Danxia groups and Luo Buddha Walled group, so that Nanxiong base layer containing dinosaur fossils exposed to the surface, this entire process is a lengthy process.
南雄盆地聚集了各种爬行动物，在河湖沿岸地带繁衍生息，四周山地突起，大量风化碎屑被河流带到盆地中沉积下来，一些死亡的恐龙遗体或已被洪水吞噬的恐龙及埋藏在土层中的恐龙蛋和留在河湖泥沙层的恐龙脚印等等，随同沉积物被深深埋藏于地下，经长期的石化过程而变成各种化石，如恐龙骨骼、恐龙蛋及遗迹化石；白垩纪末，受最后一期燕山运动的影响，南雄盆地发生微弱的断裂活动和短期抬升，南雄群地层遭受一段时间的侵蚀；至新生代古新世中期，南雄盆地再次下沉，其上接受早第三纪罗佛寨群河湖相及洪积相堆积；始新世初，该盆地又有短暂抬升并造成沉积间断，后下沉又接受丹霞洪积相与河湖相堆积；渐新世末，受喜山运动影响，整个盆地与粤北其他地区一样，普遍抬升，并伴随抬斜断裂活动，该盆地成为侵蚀区，盆地南缘因抬升较高，首先侵蚀掉上覆丹霞群和罗佛寨群，使南雄群含恐龙化石层暴露于地表，这整个过程是一个漫长的过程。
During the Eocene, this region was located at much the same latitude it is today, though global climate was more equable.
在始新世期间，这个地区是位于今天的同一纬度，可是那是全球气候差异变化比较小。
Thermo-chronological diagram of minerals from milonite shows 4 phases of thrusting in 191-174Ma, 174-144Ma, 109Ma and 44Ma of WNT, lead to 0.4mm/a, 0.22mm/a and 0.2mm/a uplifting respectively. It is concluded that thrusting in 174-173Ma, 109Ma and 44Ma of WNT were caused by southward subduction of Bangoin-Nujiang Oceanic Plate in Early-Meso Jurassic, northward subductions of Namco-Yongzhu intra-island arc Oceanic Plate and Yaluzangbu Oceanic Plate in Late cretaceous and close of Yaluzangbu Ocean and its following continental collision in Early Eocene respectively.
认为侏罗纪早中期（173-174Ma）、晚白垩世（约109Ma）、古近纪早期（约44Ma）WNT的逆冲推覆构造运动分别与班公—怒江古大洋板块南向俯冲、纳木错—永珠残余洋盆的萎缩和雅鲁藏布江古大洋板块的北向俯冲、新特提斯残余古大洋板块北向俯冲闭合及随后印度—欧亚陆—陆碰撞存在动力学成因联系。
The results revealed that Relu flora (MAT=17.3±3.7℃), A part of Yilan flora (MAT=18.2±2.9℃), and Liuqu flora (MAT=22.7±2.3℃), from Early Eocene to early Middle Eocene, corresponded to hot climate.
分析结果显示，热鲁植物群（年均温17.3±3.7℃）、依兰植物群A段（年均温18.2±2.9℃）和柳区植物群（年均温22.7±2.3℃）反映了早始新世至中始新世早期气温较高。
Whichever way you look at the Eocene enigma, it is bad news for life on Earth.
无论用何种途径来观察始新世温室的这个谜，都对地球上生命带来不好的消息。
He hadn't really wanted to spend a cold, miserable afternoon discussing yeast from the Eocene.
他并不是真的想消磨一个寒冷、悲惨的下午来探讨来自创新世的酵母。