Lunar and Terrestrial Planet Formation in the Grand Tack Scenario
Seth A. Jacobson, Alessandro Morbidelli

TL;DR
This study uses N-body simulations within the Grand Tack model to explore how initial disc conditions influence terrestrial planet formation, concluding that Mars-sized embryos dominated the early disc and the Moon formed 60-130 million years after solids first appeared.
Contribution
It provides new insights into the initial conditions of planet formation by coupling giant planet migration with terrestrial accretion in the Grand Tack scenario.
Findings
The timing of the last giant impact depends on the embryo-to-planetesimal mass ratio.
The size of the lunar impactor is linked to the initial embryo mass.
The Moon-forming event likely occurred 60-130 million years after initial solids.
Abstract
We present conclusions from a large number of N-body simulations of the giant impact phase of terrestrial planet formation. We focus on new results obtained from the recently proposed Grand Tack model, which couples the gas-driven migration of giant planets to the accretion of the terrestrial planets. The giant impact phase follows the oligarchic growth phase, which builds a bi-modal mass distribution within the disc of embryos and planetesimals. By varying the ratio of the total mass in the embryo population to the total mass in the planetesimal population and the mass of the individual embryos, we explore how different disc conditions control the final planets. The total mass ratio of embryos to planetesimals controls the timing of the last giant (Moon forming) impact and its violence. The initial embryo mass sets the size of the lunar impactor and the growth rate of Mars. After…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
