Constraints on terrestrial planet formation timescales and equilibration processes in the Grand Tack scenario from Hf-W isotopic evolution
Nicholas G. Zube, Francis Nimmo, Rebecca Fischer, Seth A. Jacobson

TL;DR
This study uses N-body simulations and Hf-W isotopic modeling to investigate how the Grand Tack scenario affects terrestrial planet formation timescales and core-mantle equilibration, revealing challenges to rapid accretion models.
Contribution
It combines collisional simulation data with isotopic evolution models to constrain impactor core mixing and accretion timescales in the Grand Tack scenario.
Findings
Faster planet formation in Grand Tack due to higher planetesimal density.
Significant core-mantle re-equilibration (k_core ≥ 0.6) needed to match Earth's tungsten isotopic composition.
Rapid accretion models may be inconsistent with core mixing constraints.
Abstract
We examine 141 N-body simulations of terrestrial planet late-stage accretion that use the Grand Tack scenario, coupling the collisional results with a hafnium-tungsten (Hf-W) isotopic evolution model. Accretion in the Grand Tack scenario results in faster planet formation than classical accretion models because of higher planetesimal surface density induced by a migrating Jupiter. Planetary embryos that grow rapidly experience radiogenic ingrowth of mantle W that is inconsistent with the measured terrestrial composition, unless much of the tungsten is removed by an impactor core that mixes thoroughly with the target mantle. For physically Earth-like surviving planets, we find that the fraction of equilibrating impactor core is required to produce results agreeing with observed terrestrial tungsten anomalies (assuming equilibration with relatively large…
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