Preliminary Phanerozoic polar wander paths for the North and South China blocks
Preliminary Phanerozoic polar wander paths for the North and South China blocks
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DOI：
10.1038/313444a0
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发表时间：
1985-02
期刊：
影响因子：
64.8
通讯作者：
Jin-lu Lin;Michael D Fuller;Wen-you Zhang
中科院分区：
文献类型：
--
作者：
Jin-lu Lin;Michael D Fuller;Wen-you Zhang
华北和华南地块的极移轨迹表明：（1）在古生代时，它们都是冈瓦纳大陆的一部分;（2）华北地块在晚二叠世增生到西伯利亚;（3）华南地块在中三叠世至早侏罗世增生到华北地块。通过与欧亚大陆北方和华南块体极移路径的比较，发现它们之间的相对运动超过4,000 km。
Polar wander paths for the North and South China blocks suggest that (1) both were parts of Gondwana in the Palaeozoic, (2) the North China block accreted to Siberia in the late Permian and (3) the South China block accreted to the North China block in the middle Triassic to the early Jurassic. Comparison of the polar wander path for the South China block with that for northern Eurasia suggests that relative motion of over 4,000 km has occurred between them.