冈瓦纳古陆最终解体了，成为我们今天知道的大陆。
Eventually Gondwana broke apart, becoming the continents we know today.
它被认为是冈瓦纳大陆与欧亚大陆长期相互作用的结果。
The Plateau resulted from the interaction of the Gondwanaland and the Eurasia continent in a long time.
当时的欧亚大陆虽大致在现今位置，而冈瓦纳大陆尚在赤道附近，并且是“内部分隔”的微大陆。
At that time, the position of Eurasia was almost the same as today, but Gondwana was near the equator and was an "internal separation" microcontinent then.
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