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震旦纪大冰期后开始了显生宙。After the Sinian Great Ice Age, the Phanerozoic started.

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.

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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.

它们构成中国大陆显生宙地壳生长的基本方式。These modes are the basic modes for the Phanerozoic continental growth of the continent of China.

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.

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.

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它的边界在东北、西北和西部由断层和新元古代和显生宙沉积盆地所圈定。Its margins are delineated to the northeast, northwest and west by faults and Neoproterozoic and Phanerozoic sedimentary basins.

在显生宙地球历史中，如此巨大且迅速的火山作用普遍被认为是巨大种群灭绝的原因。Such voluminous and rapid volcanic activities in Phanerozoic have commonly been thought to be a cause for zoobiocenose extinction.

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.

环斑花岗岩既可以出现于从太古代到显生宙的各个地质时期，也可以产生于造山带中。Recent studies show, however, that rapakivi granites can be formed in age from Archaean to Phanerozoic and can even occur in orogen.

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.

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秦岭-大别造山带的发展演化与全球联合古陆的形成与裂解十分相似。The development and evolution of Qinling-Dabie orogenic belt is quite similar to the formation and splitting of the Pangea since Phanerozoic eon.

在成因上同时与太古宙绿岩建造和显生宙花岗岩类有关的一系列金矿床构成了地台区特有的金矿床系列。A series of gold deposits related to both Archaen green stone formation & Phanerozoic granites constitute the characteristic gold deposit series in platforms.

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.

晚泛非期变质事件年龄的确定对重塑晚前寒武纪-显生宙早期麻山杂岩和佳木斯地块的古地理位置具有重要意义。The Late Pan-African age of metamorphism is important when considering the location of the Mashan Complex and Jiamusi Massif during the late Precambrian to early Phanerozoic.

二叠—三叠纪之交的生物大绝灭是显生宙以来地史转折期中最显著的集群绝灭事件，它是地学界长期关注的热点之一。The Permian-Triassic mass extinction is the most significant mass extinction event in the Phanerozoic transitional stages, and it's focus which geologists concern for a long-time.

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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.

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.

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.