4 citations · 4 across the 5 of their papers we have counts for
5 papers
Magnitude of stable iron isotope fractionation limited by multiple stages of terrestrial core formation
Gabriel Nathan, Seth A. Jacobson
One proposed mechanism for generating iron isotopic differences between planetary mantles and chondrites is metal-silicate equilibration during terrestrial core formation. Prior st…
Oxidation Constraints on Terrestrial Planet Formation from a Ring
Katherine I. Dale, Alessandro Morbidelli, Gabriel Nathan +3
The present-day solar system comprises meteorites with varying oxidation levels, derived from different parent bodies. Previous studies (e.g. Rubie et al., 2011) of the partitionin…
Tungsten isotope evolution during Earth's formation and new constraints on the viability of accretion simulations
D. C. Rubie, K. I. Dale, G. Nathan +5
The Hf-W isotopic system is the reference chronometer for determining the chronology of Earth's accretion and differentiation. However, its results depend strongly on uncertain par…
An improved model of metal/silicate differentiation during Earth's accretion
K. I. Dale, D. C. Rubie, M. Nakajima +5
We improved the algorithm presented in Rubie et al. (2015) to model the chemical evolution of Earth driven by iron/silicate differentiation during the planet's accretion. The press…
Constraining the Origin of Mars via Simulations of Multi-Stage Core Formation
Gabriel Nathan, David C. Rubie, Seth A. Jacobson
It remains an elusive goal to simultaneously model the astrophysics of Solar System accretion while reproducing the mantle chemistry of more than one inner terrestrial planet. Here…