Plants and animals from the Mesozoic era were unable to survive in the Cenozoic era.
中生代的动植物在新生代无法生存。
The fossil record suggests that there was an abrupt extinction of many plants and animals at the end of the Mesozoic era.
化石记录表明，在中生代末期，许多动植物突然灭绝。
The rift development slowly halted some 250 to 245 million years ago, around the beginning of the Mesozoic Era.
这些裂缝的活动在大约2.5-2.45亿年前，即中生代初期逐渐停止了。
Dinosaur, any of various extinct, often gigantic, carnivorous or herbivorous reptiles of the orders saurischia and ornithischia that were chiefly terrestrial and existed during the Mesozoic era.
恐龙一种，主要生活在中生代时期的陆栖动物，是庞大的食肉或食草爬行类动物，属龙盘目与鸟盘目，已绝种。
It is a product of volcanic rocks of the mesozoic era over-saturated with silica and rich in potash. it can be compared with geode natrolite that producedin alkaline basalt series of the cenozoic era.
它是中生代硅酸过饱和并富钾质的火山岩系的产物，其意义可与产于新生代碱性玄武岩系中的晶洞钠沸石对比。
Mammals arose from a fairly primitive reptile in the Mesozoic era.
哺乳类起源于中生代宛若原始的爬虫类。
But by mistake, they end up traveling through time to the actual Mesozoic era and come face to face with real meat-eaters!
可是阴差阳错，他们竟然穿越时空来到了远古的中生代，遇上了真正的食肉龙！
An era of geologic time, from the end of the Precambrian to the beginning of the Mesozoic, or from about 570 to about 225 million years ago.
古生代是地质时期的一个时代，从前寒武纪末开始，到中生代初，大约从5.7亿年前到2.25亿年前。
The gingko tree is a survivor from the Mesozoic Era.
银杏是中生代幸存下来的植物。
These geologic formations date to the Mesozoic era, when layers of sedimentary limestone accumulated under water.
这些地质形成日期中生代时期，当层沉积的石灰岩积累下的水。
Dinosaurs vanished from the earth at the end of the Mesozoic Era.
中生代末期，恐龙从地球上消失了。
The exhalation-spout type deposits of the early Paleozoic era and the orogenic type deposits of the late Paleozoic to early Mesozoic era are the most important deposit groups.
早古生代时期的喷气喷流型矿床组合和晚古生代—早中生代时期的造山型矿床组合最为重要。
Many collisions of considerable size and periods of supervolcanism occurred early in the Mesozoic era.
在中生代以前发生了许多次大规模的碰撞与大型的火山喷发。
Mesozoic era granites in northwestern Fujian can be generally classified into two types: remelting type and syntectic type.
闽西北中生代花岗岩总体上可分为重熔型和同熔型两种类型。
Like the Palaeozoic Era, the Mesozoic Era has been divided into smaller units of geological time called period.
如同古生代一样，中生代也可划分成一些叫纪的较小的时间单位。
It is supposed that the NE structural belt along southeast margin of Hannan Massif belongs to the nappe formed after Mesozoic Era in terms of Hujiaying nappe.
从胡家营的推覆构造可推知汉南地块东南缘北东向构造带，应属于中生代以来所形成的推覆体构造。
The purpose of this paper is to present certain facts relating to magmatism and metallization in the northern Taihang Mountains during Mesozoic era.
太行山北段中生代岩浆活动频繁，成矿作用强烈，岩体和岩石种类、矿点和矿化类型都很多。
Formation and emplacement of gabbro inclusion are related to the subduction of Philippines 'plate underthrusting downwards into China continent since Mesozoic Era.
辉长岩的形成、侵位，与菲律宾板块自中生代以来向中国大陆俯冲作用有关。
The three major rock systems of the Mesozoic era, the Triassic, Jurassic and the Cretaceous are notable oil-producing systems.
中生代的三大岩系：三叠系、侏罗系和白垩系，是三个著名的产油岩系。
Songliao basin is a expanding and rifted basin which was formed in Mesozoic era.
松辽盆地是一中生代形成的伸展裂陷盆地。
The ultrabasic rocks of Mesozoic Caenozoic era have been found in the northeastern Jiangxi Province.
赣东北地区发现有中-新生代超基性岩。
The geology of the surrounding areas of east China sea basin indicates that Marine environment: existed during middle-late Mesozoic era and late Palaecz - oic era.
东海盆地周边地质表明存在有中生代、古生代地层，并有过海相沉积环境。
In Mesozoic era, the formation and evolution of the Mesozoic Lanping Simao basin were controlled by the Tethys tectonic zone.
在中生代，该盆地的形成与演化受特提斯构造带的控制。
The wall rocks of gold deposits located in Zhaoyuan gold mineralization area were rooted in metamorphic rocks in Jiaodong rock group in Archaean era and granites in Mesozoic era.
山东招远金矿集中区金矿床的围岩为新太古代胶东岩群变质岩和中生代花岗岩。
Photo Gallery: Jurassic Period An Allosaurus tramps through a Mesozoic-era forest in this artist's depiction.
侏罗纪时代图片集。一只古生异龙践踏通过一个中生代时期的森林在这方面艺术家的写照。
It firstly proposed that the Chaidamu tiny plate was affected by the Tarim plate in Mesozoic Era, but it was mainly influenced by Qiangtang plate and the south plate in Cenozoic Era.
本文首次提出了柴达木微板块在中生代主要受塔里木板块的影响，而新生代主要受羌塘板块及其以南板块的影响。
It firstly proposed that the Chaidamu tiny plate was affected by the Tarim plate in Mesozoic Era, but it was mainly influenced by Qiangtang plate and the south plate in Cenozoic Era.
本文首次提出了柴达木微板块在中生代主要受塔里木板块的影响，而新生代主要受羌塘板块及其以南板块的影响。
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