震旦纪大冰期后开始了显生宙。
显生宙期间，中国南部的构造属性曾几经转化。
The tectonic nature of southern China has Changed again and again in the Phanerozoic.
地球上有两套完全不同的造山系统一直存在于显生宙。
Two fundamentally different orogenic systems have existed on Earth throughout the Phanerozoic.
显生宙可划分为三个时期——依次经历古生代、中生代和新生代。
The Phanerozoic is divided into three eras — starting with the earliest, these are the Paleozoic, Mesozoic, and Cenozoic.
显生宙可划分为三个时期——依次经历古生代、中生代和新生代。
The Phanerozoic is divided into three eras -starting with the earliest, these are the Paleozoic, Mesozoic, and Cenozoic.
年轻的钕同位素模式年龄表明该区存在新元古—显生宙的地壳增生。
The young Nd model ages suggest a significant crustal growth in the period of Neoproterozoic-Phanerozoic.
该研究从另一个侧面证明中亚造山带存在一定规模的显生宙陆壳生长。
This study provides new evidence for continental crustal growth in the central Asian orogenic belt during the Phanerozoic.
显生宙的海绿石，多年来研究的结果表明海绿石发育在慢速弱还原环境。
The Phanerozoic glauconites in this study show that they were formed in an environment of weak reduction and low sedimentation.
地球的历史可分为四个时期——依次经历冥古代、太古代、元古代和显生宙。
The history of Earth is divided into four eons - starting with the earliest, these are the Hadean, Archean, Proterozoic, and Phanerozoic.
地球的历史可分为四个时期——依次经历冥古代、太古代、元古代和显生宙。
The history of Earth is divided into four eons —starting with the earliest, these are the Hadean, Archean, Proterozoic, and Phanerozoic.
本组为评估中元古代生命状况、古环境和前显生宙生物地层提供了重要的生物信息。
This Formation provides important paleobiological information from which to assess status of Mesoproterozoic life, and to evaluate paleoenvironmental conditions and pre_Phanerozoic biostratigraphy.
阿尔泰造山带是中亚地区显生宙大陆地壳增生明显的地区之一，蕴藏丰富的矿产资源。
The Altai orogeny, as one of notable crustal accretion areas, is famous for its abundant mineral deposits.
显生宙以来处于劳亚大陆与冈瓦纳大陆之间，纪录了古亚洲洋、古特提斯洋的演化历程。
It is laid between the Laurisia land and the Gondwanaland during the Phanerozoic and recorded the evolutional process of Palaeo-Asia Ocean and Palaeo-Tethyan Ocean.
统一陆壳也是显生宙以来逐步形成的：主要经历了加里东和华里西-印支两大构造阶段。
The Qinghai crust was gradually collaged during the Paleozoic and mainly underwent Caledonian and Hercynian-Indosinian tectonic events.
UHPM记录了显生宙俯冲-碰撞造山带早期碰撞过程中的低热流梯度及陆壳的深俯冲作用。
HPM-UHPM registers the low thermal gradients and deep subduction of continental crust during the early stage of the collision process in Phanerozoic subduction-to-collision orogens.
最早的生命迹象发现存在于距今38亿年的太古代，但是地球上的生命在显生宙之前并不丰富。
Evidence for life has bee found in the Archaean about 3.8 billion years ago, but life did not become abundant until the Phanerozoic.
部分太古宙绿岩带由不同的构造单元拼合而成，并发育不同于显生宙蛇绿岩的大洋壳岩石组合。
Some Archean greenstone belts represent collages of allochthonous fragments, among which oceanic crust slices are identified with characteristics distinct from the Phanerozoic ophiolites.
这显然与北部拉张条件下形成登封绿岩带的环境不同。也有别于显生宙之后发生附冲作用的环境。
Clearly, it is different from Archean greenstone belt, for example, the Dengfeng greenstone belt located adjacent to it on the north.
群集出现常伴随着群集消失，这可见于显生宙许多发生过灾变事件的纪一级或其他级别的地层界限附近。
Mass appearance is usually accompanied by mass disappearance, which may be found near many interperiod boundaries or other boundaries of the Phanerozoic where catastrophic events happened.
反过来讲，这个时代是显生宙(Phanerozoic)[4]最为年轻的构成部分——在地球5.4亿年以来的历史中，那些含有复杂生命体的化石都可以在这个时代找到。
This era in turn marks the most recent part of the Phanerozoic aeon, the 540m-year chunk of the Earth's history wherein rocks with fossils of complex organisms can be found.
反过来讲，这个时代是显生宙(Phanerozoic)[4]最为年轻的构成部分——在地球5.4亿年以来的历史中，那些含有复杂生命体的化石都可以在这个时代找到。
This era in turn marks the most recent part of the Phanerozoic aeon, the 540m-year chunk of the Earth's history wherein rocks with fossils of complex organisms can be found.
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