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本文计算了1698个岩石和矿物的氧平均体积,从中得出结论,玻璃质喷出岩V_0为22.5 ~3,半晶质喷出岩V_0为21.5 ~3,金晶质喷出岩和从花岗岩到辉长岩的侵入岩V_0平均为20.6 ~3。按照地球圈层模型,上地壳V_0为20.8 ~3下地壳若为辉长岩,则V_0与上地壳基本相同,若为角闪岩或闪长岩成分的石榴石麻粒岩,则V_0为18.8 ~3,根据地幔包体和高温高压实验资料,计算出上地幔V_0为17.7 ~3。这些都是分层守恒的常数,并与等大球任意堆积的各个堆积系数相对应。
In this paper, the average oxygen volume of 1698 rocks and minerals was calculated. It was concluded that the V_0 of vitreous extrusive rock was 22.5-3, that of semi-crystalline rock was 21.5-3, The gabbro intrusive rock V_0 averaged 20.6 ~ 3. According to the geosphere model, if the upper crust V_0 is 20.8 ~ 3 and the lower crust is gabbro, then V_0 is basically the same as the upper crust, with a V_0 of 18.8 for the garnet granulites of amphibolite or diorite According to the data of mantle inclusions and high temperature and high pressure, V_0 of upper mantle is calculated to be 17.7 ~ 3. These are constants that are conserved hierarchically and correspond to the individual packing factors that are arbitrarily stacked in the same ball.