1)Late Mesozoic中生代晚期
1.Late Mesozoic and Paleogene Basalts and Deep-Derived Xenocrysts in Eastern Liaoning Province, China: Constraints on Nature of Lithospheric Mantle;辽东中生代晚期和古近纪玄武岩及深源捕虏晶——对岩石圈地幔性质的制约
2.Division of the Late Mesozoic strata in Zhejiang;论浙江中生代晚期地层划分
3.Taxonomy of Fossil Ephemeroptera from Late Mesozoic in China, with Comments on Succession of Aquatic Insect Community中国中生代晚期蜉蝣目化石研究及水生昆虫群落演替分析
英文短句/例句
1.Taxonomy of Fossil Ephemeroptera from Late Mesozoic in China, with Comments on Succession of Aquatic Insect Community中国中生代晚期蜉蝣目化石研究及水生昆虫群落演替分析
2.AQUATIC COMMUNITY SUCCESSION AND ENVIRONMENTAL CHANGES OF LATE MESOZOIC IN NORTHERN CHINA中国北方中生代晚期水生昆虫群落演替与环境变迁
3.Taxonomy of Fossil Palaeontinidae from the Late Mesozoic in Northeast China (Insecta: Homoptera: Cicadomorpha)中国中生代晚期古蝉科昆虫化石研究（同翅目：蝉亚目）
4.There was an orogenic belt called the Cathaysian continental marginal orogenic belt in late Mesozoic along the present northern margin of the South China Sea.南海北部陆缘在中生代晚期曾形成宏伟的华夏陆缘造山带。
5.DISCOVERY OF LATE MESOZOIC MAGMATIC ROCKS IN ORDOS ANCIENT CONTINENT NUCLEUS AND ITS GEOLOGICAL IMPLICATION鄂尔多斯古陆核内部中生代晚期火山岩的发现及其地质意义
6.Ecostratigraphic subdivision revealed a general pattern of basin evolution which reappears in many other sections of Northern Hebei Province.生态地层划分的结果显示了中生代晚期在冀北许多地区具有代表性的盆地演变的一般模式。
7.Orggenic Processes of the Inner Mongolia-Yanshan Area in Eastern China during the Late Late Paleozoic-Mesozoic;中国东部内蒙—燕山地区晚古生代晚期—中生代的造山作用过程
8.Late Mesoproterozoic to Paleozoic tectonothermal events in the Eastern Segment of the Central Tianshan Tectonic Zone of Northwestern China:Constraints from SHRIMP zircon geochronology.中天山东段中元古代晚期—古生代构造-热事件:SHRIMP锆石年代学证据
9.There are at least nine physiographic cycles in the middle reaches of the Yellow River during the Late Cenozoic Era.在晚新生代黄河中游至少存在九个地文期旋回。
10.On the Poor Scholars Social Intercourse in the South of the Changjiang River during the Middle and Late Ming Dynasty;明代中晚期江南地区贫士的社会交往生活
11.Returned Students in Late Qing Dynasty lately and the Origin of Modern Chinese Systemetic Learning;晚清时期的留学生与中国现代学术的起源
12.LATE MESOPROTEROZOIC MICROFOSSIL ASSEMBLAGE ON NORTHERN SLOPE OF EASTERN QINLING MOUNTAINS, CHINA: A NEW WINDOW ON EARLY EUKARYOTES东秦岭北坡中元古代晚期微体生物群——一个早期生命的新窗口
13.Basin Evolution and Geodynamics of Northwestern upper Yangtze Block during Late Paleozoic to Mesozoic上扬子地块西北缘古生代晚期—中生代的盆地演化及地球动力学
14."Late Imperial China" and "Early Modern China"“晚期帝制中国”与“早期现代中国”
15.RESEARCH ON DATE MESOZOIC FLORAS AND ITS PALEOECOLOGY ON THE EAST MARGIN OF SONGLIAO BASIN, JILIN PROVINCE吉林省松辽盆地东缘晚期中生代植物群及其古生态研究
16."Towards the end of the Old Stone age later than 50,000 years ago, homo sapiens were living in almost all corners of China"旧石器时代晚期，约5万年前，智人已生息在中国的各个角落。
17.On Late Neolithic Livelihood Economy and Population Pressure in the Middle Yangtze River Valley;论长江中游地区新石器时代晚期的生计经济与人口压力
18.The status and role of the Ling-nan students abroad in the late Qing period;晚清时期岭南出国留学生在中国近代留学史上的地位与作用
相关短句/例句
mid-late Mesozoic period中生代中晚期
3)the middle stage of Late Paleozoic晚古生代中期
1.4 Ma) of biotite shows that the rock is formed in the middle stage of Late Paleozoic era.4Ma,属晚古生代中期的花岗岩。
4)Late Paleozoic-Mesozoic古生代晚期-中生代
5)middlelate Mesozoic extensional tectonics中生代中晚期伸展构造
6)late Mesozoic晚中生代
1.Strata Sequence of the Late Mesozoic and Basin Evolution in the Southeastern Liaoning;辽东南地区晚中生代地层序列与盆地演化规律
2.A new case of Late Mesozoic crust-mantle interaction in eastern Zhejiang:Geochronology and geochemistry of the Ru ao diabase-granite composite intrusions;浙东晚中生代壳幔相互作用的新例证——新昌儒岙辉绿岩-花岗岩复合岩体的年代学与地球化学
3.A review on the late Mesozoic extensional tectonics on the eastern North China Craton;华北东部晚中生代伸展构造作用
延伸阅读
中生代中生代（距今约2.5亿年～距今约6500万年）MesozoicEra显生宙第二个代，晚于古生代，早于新生代。这一时期形成的地层称中生界。中生代名称是由英国地质学家J.菲利普斯于1841年首先提出来的，是表示这个时代的生物具有古生代和新生代之间的中间性质。自老至新中生代包括三叠纪、侏罗纪和白垩纪。中生代时，爬行动物（恐龙类、色龙类、翼龙类等）空前繁盛，故有爬行动物时代之称，或称恐龙时代。中生代时出现鸟类和哺乳类动物。海生无脊椎动物以菊石类繁盛为特征，故也称菊石时代。淡水无脊椎动物，随着陆地的不断扩大，河湖遍布的有利条件，双壳类、腹足类、叶肢介、介形虫等大量发展，这些门类对陆相地层的划分、对比非常重要。中生代植物，以真蕨类和裸子植物最繁盛。到中生代末，被子植物取代了裸子植物而居重要地位。中生代末发生著名的生物绝灭事件，特别是恐龙类绝灭，菊石类全部绝灭。有人认为生物绝灭事件与地外小天体撞击地球有关，但真正原因有待进一步研究确定。古生代末期，联合古陆的形成，使全球陆地面积扩大，陆相沉积分布广泛。中生代中、晚期，联合古陆逐渐解体和新大洋形成，至中生代末，形成欧亚、北美、南美、非洲、澳大利亚、南极洲和印度等独立陆块。并在其间相隔太平洋、大西洋、印度洋和北极海。中生代中、晚期，各板块的漂移加速，在具有俯冲带的洋、陆壳的接触带上俯冲、挤压，导致著名的燕山运动（或称太平洋运动），形成规模宏大的环太平洋岩浆岩带、地体增生带和多种内生金属、非金属矿带。中生代气候总体处于温暖状态，通常只有热带、亚热带和温带的差异。
