潮汐摩擦力
- 网络tidal friction
潮汐摩擦力-
随着潮汐摩擦力和地球体积的增大，地球自转角速度变慢。
Because of tidal friction and aggrandizement of the earth 's volume , the earth 's rotation angular velocity slows down .
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通过分析各种地壳运动假说，提出了地幔胀缩力和重力是地壳运动的主要动力来源，地球自转离心力和潮汐摩擦力是地壳运动的次要动力来源。
This paper holds that Earth 's gravity , expanding and contracting pressures of mantle are major dynamic sources for crustal movement , while centrifugal force from of the Earth 's rotation and tidal frictional force are secondary dynamic source .