Comparison of the Earth's Craters and the Moon's Basins

Mathematics – Logic

Scientific paper

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Scientific paper

Two classes of planetary concentric features have much in common.
Primarily, they both outline the geological framework of their bodies
and occupy similar time-space positions. Time intervals of their
formation are close to each other (Moon: 4.4 - 3.8, Earth: 4.3 - 3.5
b.y.). They reveal similarity in structure and mantle magmatism.

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