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... assumes that angular momentum of the Earth-Moon system L in Eq.2 is a constant. Using Eq.1 for ω with step of 250Ma is computed Earth-Moon distance R in geological history of the Earth (Fig.5). As is the above mentioned R is non linear function of time. ...
Context 2
... data for S cr (Table 1) is computed L(500). With Eq.2 and data for ω(500) (from Eq.1) is computed R(500) etc. Figure 5 shows R-0 and R-1-crust models. Data from this model shows that R has a minimum at 1,75GaBP. ...
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