Ward W R
Science. 1975 Aug 1;189(4200):377-9. doi: 10.1126/science.189.4200.377.
The orientation of the lunar spin axis is traced from the early history of the earth-moon system to the present day. Tides raised on the earth by the moon have caused an expansion of the lunar orbit. Tides raised on the moon by the earth have de-spun the moon to synchronous rotation and driven its spin axis to a Cassini state-that is, in a coprecessing configuration, coplanar with the lunar orbit normal and the normal to the Laplacian plane (which is at present coincident with the normal to the ecliptic). This combination of events has resulted in a complex history for the lunar spin axis. For much of the period during which its orbital semimajor axis expanded between 30 and 40 earth radii, the obliquity of the moon was of order 25 degrees to 50 degrees . In fact, for a brief period the obliquity periodically attained a value as high as 77 degrees ; that is, the spin axis of the moon was only 13 degrees from lying in its orbit plane.
月球自转轴的方向从地月系统的早期历史追溯到如今。月球在地球上引起的潮汐导致了月球轨道的扩张。地球在月球上引起的潮汐使月球自转减速至同步自转,并将其自转轴驱动到卡西尼状态,即处于共旋进构型,与月球轨道法线和拉普拉斯平面法线共面(目前与黄道法线重合)。这些事件的综合作用导致了月球自转轴的复杂历史。在其轨道半长轴在30至40个地球半径之间扩张的大部分时期,月球的倾角约为25度至50度。事实上,在一段短暂时期内,倾角周期性地达到高达77度的值;也就是说,月球的自转轴与它的轨道平面仅相差13度。