摘要
地球在漫长发展演化过程中,q、μ_n′的变化规律是内外动力地质联合作用的结果,是导致地球分异的动力;月球的q、μ__n′变化不大是因漫长的化学停滞作用造成的,是缺乏內外动力地质联合作用的结果;陨石及其系列的形成,有如地球上的岩浆结晶作用一样,遵循晶格能依次增大的规律,q、μ_n′多样性反映来自小行星带的陨石物质成分的不均一。 地球、月球和陨石的q^(2/3)+μ_n′^(2/3)=82.23^(2/3)函数关系成立,表明它们从原始太阳星云中产生的同一性,作为太阳系独立成员的同时性,q、μ_n′的差异可能反映原始太阳星云物质的不均一性。
In the very long process of the development and evolution of the earth, the laws of changes in q and μ′_n are the results of the combined geological functions of inner and outer powers, and are the power leading to the earth's differentiation. The changes in q and μ′_n on the moon are not so great, which is caused by the very long chemical stagnation and by lacking the combined geological functions of inner and outer powers. The formation of meteorites and their series follows the law that their crystal lattice energy increases in proper order, just the same as the crystallization of magma on the earth. The variety of q and μ'_n mirrors the heterogeneity of meteorites' compositioncoming from the minor planet belt. The functional relation of 82.23^(2/3) is tenable to the earth, the moon and meteorites, which indicates the identity of their generating from original solar nebula and the simultaneity as the independent members of the solar system. The difference of q and μ'_n may reflect the heterogeneity of original solar nebula.
出处
《西南石油学院学报》
CSCD
1991年第3期21-28,14,共9页
Journal of Southwest Petroleum Institute
关键词
地球化学
地球
月球
陨石
能量
The earth
The moon
Meteorite
Energy
Geochemistry
