On the evolution of the protolunar disc

William R Ward1

  • 1Planetary Science Directorate, Southwest Research Institute, Boulder, CO 80027, USA ward@boulder.swri.edu.

Summary

This study models a post-impact protolunar disc, revealing a stratified structure with a stable vapor layer and an unstable magma layer. The magma layer spreads viscously over years, influencing accretion and moonlet formation before vapor depletion.

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