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盘古大陆, 泛大陆
a supercontinent that existed during the late Paleozoic and early Mesozoic eras, comprising most of Earth's landmasses fused together before breaking apart into the continents we recognize today
- Pangaea was a vast supercontinent that formed about 335 million years ago.
盘古大陆是一个大约在3.35亿年前形成的广阔超大陆。
- The assembly of Pangaea resulted from the convergence and collision of several smaller landmasses.
盘古大陆的组装是由于几个较小的陆块的汇聚和碰撞造成的。
- Pangaea's existence is a key concept in plate tectonics, explaining the movements of Earth's lithospheric plates.
盘古大陆的存在是板块构造学中的一个关键概念，解释了地球岩石圈板块的运动。
- The breakup of Pangaea began around 175 million years ago during the Mesozoic Era.
盘古大陆的分裂始于大约1.75亿年前的中生代。
- Pangaea included present-day continents like North America, South America, Africa, Europe, Antarctica, Australia, and Asia.
盘古大陆包括了现今的各大洲，如北美洲、南美洲、非洲、欧洲、南极洲、澳大利亚和亚洲。
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