The subsequent Rhems Formation is apparently the product of rapid sediment accumulation during a short period of time in the early Paleocene.
之后，Rhems的形成是古新世短时期快速沉积的结果。
The ultimate extinction of the dinosaurs 6300 years ago in the Mesozoic and Cenozoic Tertiary Paleocene.
恐龙最终灭绝于6300万年前的新生代第三纪古新世。
In the latter part of the Paleocene, large angiosperm fruits and seeds evoled and diversified.
在古新世后半期，大型种子植物的果实和种子进化和多样化，与此同时，食用果实和种子的哺乳动物也发生进化以及多样化。
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。
The paleontogical history of the cat can be traced back to the great diversification of mammals in the Paleocene epoch, at the beginning of the Cenozoic era, over 60 million years ago.
猫的古生物学起源可以追溯到六千万年前，此时正值新生代之初的古新世时期，这一时期哺乳动物开始了大分化。
Kuqa Thousand-Buddha Grottoes in Dunhuang and the blacksmith's groove Tertiary Paleocene formation discovered in Central Populus fossil, Suanqi Lai has at least 6, 500 years of history.
在库车千佛洞和敦煌铁匠沟的第三纪古新世地层中部发现了胡杨的化石，算起来至少也有6500万年的历史了。
It is the first time to apply this method to study sedimentary facies of the Paleocene-Miocene in the Qaidam Basin.
这是首次将定量的沉积相研究方法应用于柴达木盆地的古新统至中新统。
A large number of fossils of more than 50 species of Mammalia and Reptilia(60 Ma) in the mid-late Paleocene Epoch, have been discovered in the red clastic sedimentary rocks of Qianshan Basin in over 100 sites in the south of the Tianzhu mountain area, which is universally acknowledged as one of the original places of rodents of more than 1, 700 species including present mice in the world nowadays.
天柱山南片潜山盆地红色碎屑沉积岩中，有100多个点共发现了50多个种属的哺乳动物和爬行动物化石，均系古新世中晚期化石，距今约6，000万年，被国际公认为是当今世界上1700多种包括现在的老鼠在内的啮齿类动物起源地之一。
The foreland basin phase was controlled mainly by the thrust of Qinlin-Dabie orogenic area during later Jurassic and middle Triassic; the rift basin phase is controlled by fault and deasil circumvolving with the change of stressing during Cretaceous and Paleocene, with strong magma activity; and in the depression basin phase the bas...
盆地地壳结构和小震分布及震源机制解显示地震集中在沉降最大的潜江—沔阳凹陷带附近，震源深度优势分布在15 km左右，即盆地基底附近。
Based on the analysis and sufficiency cognition of Transgression Lake of late Cretaceous and Paleocene Epoch of Subei Basin, the research is important to not only paleogeographic reconstruction of Subei basin during late Cretaceous and Paleocene Epoch but also the comment to make upon development and distribution of the source rocks and potential of oil and gas generation.
通过对苏北盆地晚白垩世－古新世海侵湖泊的确切与充分的认识分析，不仅对苏北盆地晚白垩世－古新世时期的湖盆古地理重建，而且对烃源岩的发育与分布以及生油气潜力评价都具有重要的意义。
According to ornithology experts, fossils formed in the Paleocene Epoch depict a bird species that had a curved underside.
据鸟类专家研究，古新世(地质年代，距今6500万年～距今5300万年，译者注)形成的化石描述一种具有弯曲下面（根据后面内容，可能指鸟的足，译者注）的鸟类。
Paleocene The oldest epoch of the Tertiary, 65-55million yesrs ago.
古新世：第三纪最古的年代，6500万～5500万年前。
Themain supply groundwater source of the city of Lanzhou is the aquiferof the Fanjiaping group, paleocene epoch (N_2). At present, the groundwater within the mainly exploitational area has been polluted by the natural and social environmental pollutant provenances. It must be pointed out that there still have been existing pollutant conditions effecting contamination in the groundwater and Yellow River Hence, the important thing for us to do is to strengthen the management of environmental protection...
兰州市的主要供水含水层是范家坪组含水层，开采区地下水已受到自然、社会环境污染源的显著污染，而且尚存在继续污染的污染条件，为了使地下水和黄河水免受社会污染源的污染，必须加强环境保护工作，进行必要的环境保护工程措施；为了减轻水文地球化学环境的不利因素，以满足城市饮用水量日益增加的需要，建设将现在单一的黄河河道改进为人工黄河河道网，这样，将可扩大、诱发和激发黄河对供水含水层的补给作用。
The evidences of paleontology, minerals in rocks and geochemistry can ascertain the environment of lake basin which develops during late Cretaceous and Paleocene Epoch.
苏北盆地在晚白垩世泰州组－古新世阜宁组沉积形成了以全盆地阜二段、阜四段为主，局部泰二段的富含介形虫的暗色泥岩，成为该盆地的主力烃源岩。
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。
Therefore, lacustrine deposit can only exist in the low section of the early Paleocene, and its upper section has been in brackish water and salt water environment'Coarse s...
因此湖相沉积可能仅存在于下古新统下部，下古新统上部可能已进入半咸水及至咸水的环境。
Since tha latest of cretaceous, the xiihu sag had been undergoing rifting stage during the Paleocene and the eocene, inversion stagc during the Oligocene and the miocene, and regional subsidence stage during the Pliocene and the quaternary.
晚中生代末期以来，经历了古新世-始新世的裂谷盆地阶段。渐新世-中新世的盆地反转阶段和上新世-第四纪的区域沉降阶段。
The Paleocene to Eocene inside the basin are fluvial sediments;
盆地内古新统-始新统为河流相沉积；