Constraining the composition, core sizes and thermal state of the Moon for the models of the magma ocean

Mathematics

Scientific paper

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Scientific paper

In the present work, we suggest a new model of constitution and internal
structure of the Moon. This model is based on the hypothesis of chemical
differentiation of the Moon as a result of partial melting of initially
homogeneous material (hypothetical magma ocean); it involves modern
mathematical processing of the P - and S-velocities [1, 6].

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