冈瓦纳大陆(Gondwana)形成于5×108~10×108年前的泛非运动[13216],泛大陆(Pangea)是古生代末南古陆[17],,生界分布较为有限[18]。
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Accordingly, it can be concluded that the Middle Paleozoic is a very important period in the evolution of South Qinling belt, the South China block, as well as Gondwana.
由此可见,中古生代是南秦岭,华南板块和冈瓦纳大陆地质演化过程中一个非常重要的时期。
参考来源 - 南秦岭与扬子地体西北缘志留—泥盆系碎屑锆石物源分析及构造意义·2,447,543篇论文数据,部分数据来源于NoteExpress
调研区位于冈瓦纳大陆北缘。
The research area is located in the north margin of Gondwana.
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.
数百万年前,南半球各洲组成了一个大陆,称为冈瓦纳大陆。
Millions of years ago all the southern continents formed a single landmass known as Gondwanaland.
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