| 均衡运动中的科里奥利力 |
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| 引用本文： | 杨学祥,陈殿友,孙春林. 均衡运动中的科里奥利力[J]. 大地测量与地球动力学, 1995, 0(3) |
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| 作者姓名： | 杨学祥 陈殿友 孙春林 |
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| 作者单位： | 长春地质学院 |
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| 摘 要： | 探讨地球自转的一种惯性力──科里奥利力在地壳升降运动中的作用。地壳上升时科氏力向西，地壳下降时科氏力向东，它的大小与方向可以解释太平洋两岸的构造差异。
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| 关 键 词： | 地球自转，地壳均衡，地壳运动，构造力 |
CORIOLIS FORCE IN ISOSTASY |
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| Yang Xuexiang,Chen Diangyou and Sun Chunlin. CORIOLIS FORCE IN ISOSTASY[J]. Journal of Geodesy and Geodynamics, 1995, 0(3) |
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| Authors: | Yang Xuexiang Chen Diangyou Sun Chunlin |
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| Abstract: | Coriolis force is the inertia force coming from the earth rotation. Its effect on vertical crust movement is discussed in this paper mainly.It faces the west when the crust is in lift,and it turns towards the east when the crust is in subsidence.The strength and orientation of the force can be used to explain the diffrence of the tectonic on both sides of the Pacific Ocean. |
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| Keywords: | earth rotation isostasy crustal movement tectonic force. |
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