CAJ | 학술논문

由于月球是环绕地球运行的唯一的一颗自然卫星。对月球起源的研究不仅能够发现太阳系星球卫星的形成规律。而且可以揭示字宙星系的演进规律，进而控制星球的演进。因此许多人研究过月球，但是关于月球的起源仍然是一个不解之谜。于是本文作者通过分析和研究地球的演进过程，发现了地球卫星的形成机制．即地球岩石圈在水的长期侵蚀下分裂成一些断块．有的断块外部被溶蚀成许多溶洞，而内部又变成浮石结构，以致比重很小；当共中一个这样的断块的岩基被海水蚀透。使大量的水进入地慢与炽热的岩浆接触时．就会产生巨大的爆炸，将断块炸裂成多个浮石碎块，其中有些浮石碎块在巨大的岩浆喷射力的推动下经过大而深的岩洞可获得第一宇宙速度以上的飞行速度．从而进入绕地球运行的轨道。在这些进入绕地轨道的浮石碎块中有一块体积最大的浮石碎块就是后来形成月球的雏形。后来月雏不断地吸收地球周围的残余物质而变得越来越大．并渐渐地远离地球。
유우월구시배요지구운행적유일적일과자연위성。대월구기원적연구불부능구발현태양계성구위성적형성규률。이차가이게시자주성계적연진규률，진이공제성구적연진。인차허다인연구과월구，단시관우월구적기원잉연시일개불해지미。우시본문작자통과분석화연구지구적연진과정，발현료지구위성적형성궤제．즉지구암석권재수적장기침식하분렬성일사단괴．유적단괴외부피용식성허다용동，이내부우변성부석결구，이치비중흔소；당공중일개저양적단괴적암기피해수식투。사대량적수진입지만여치열적암장접촉시．취회산생거대적폭작，장단괴작렬성다개부석쇄괴，기중유사부석쇄괴재거대적암장분사력적추동하경과대이심적암동가획득제일우주속도이상적비행속도．종이진입요지구운행적궤도。재저사진입요지궤도적부석쇄괴중유일괴체적최대적부석쇄괴취시후래형성월구적추형。후래월추불단지흡수지구주위적잔여물질이변득월래월대．병점점지원리지구。
Since the Moon is the only natural satellite of the Earth, the research on the origin of the Moon can not only find out the formation law of the satellites of solar system planets but also reveal the evolution law of galaxies in the universe. Hence many people have studied the Moon, but the origin of the Moon remains a mystery. The authors of this paper, through an analysis on the evolu- tion of the Earth, revealed the formation mechanism of the Moon, that is, some lithospheric fault blocks suffering erosion of water over long periods of time eventually developed many limestone caves, while their inner part became pumice stone, so they had low specific gravity. When the rock foundation of such a fault block was eroded so seriously that a large amount of water entered the mantle to contact super hot magma, a tremendous explosion occurred, breaking the fault block down into several pieces of pumice stone; then under the effect of strong eruption force, some pumice stones through the large and deep rock hole could achieve a speed not tess than the first cosmic speed to enter an orbit around the Earth. Among these pumice stones in the orbit, the maximal one is the young moon, which has unceasingly incorporated the remnants around the Earth to become larger and larger, and farer and fareraway from the Each,