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.
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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