摘要
从南半球大陆的海岸边缘关系,说明南半球古大陆曾位于南极附近。在地球自转减慢的附加力和 Coriolis 力的共同作用下,南半球古大陆发生了向赤道的漂移。
Based on relationship between coastlines of recent continents over the Southern hemisphere, the study shows that the ancient continents over the Southern hemisphere were around the south pole.The additional force for deceleration of the earth's rotation together with the Coriolis force have dirved the ancient continents to drift toward the equator and then spread over the Southern hemisphere.
出处
《地质科学》
CAS
CSCD
北大核心
1992年第3期305-308,共4页
Chinese Journal of Geology(Scientia Geologica Sinica)
关键词
南半球
大陆
岛屿
分布
地球
自转
Southern hemisphere
Continent drift
Additional fore
Earth's rotation
Coriolis force
