The cosmic molybdenum–ruthenium isotope correlation

By N. Dauphas, A. Davis, B. Marty, L. Reisberg. 2004

183 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Nuclear and High Energy Physics

View Paper: https://www.semanticscholar.org/paper/0c4a3fbc60358ebe1e32bbcc2514e2faaa702517

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In Astronomy and Astrophysics

1. C. Burkhardt
2. N. Dauphas
3. T. Kleine
4. B. Bourdon
5. Haolan Tang
6. C. Travaglio
7. R. Wieler
8. O. Eugster

In Nuclear and High Energy Physics

1. C. Travaglio

Citations in the corpus

• Origin of water in the terrestrial planets (2005, unknown): “However, Dauphas et al. (2004) use Ru and Mo isotopic systematics to argue against this possibility and argue for homogeneous accretion.”
• Molybdenum isotope anomalies in meteorites: Constraints on solar nebula evolution and origin of the Earth (2011, background): “(Dauphas et al., 2004).”
• Abundance, distribution, and origin of 60Fe in the solar protoplanetary disk (2012, background): “…reflecting instead inheritance of nucleosynthetic anomalies carried by presolar phases, as had been documented previously for several other elements (Dauphas et al., 2002, 2004b; Hidaka et al., 2003; Andreasen and Sharma 2006, 2007; Trinquier et al., 2007, 2009; Carlson et al., 2007; Qin et al.,…”
• Calcium-48 isotopic anomalies in bulk chondrites and achondrites: Evidence for a uniform isotopic reservoir in the inner protoplanetary disk (2014, background): “Following the approach of Dauphas et al. (2004), the isotopic anomalies in A relate to those in B through, ε j/i A = ρ j/i A − μ j/iμk/i ρ k/i A ρ q/p B − μq/pμr/p ρ r/p B c i A p Bε q/p B, (B.1) with, ρ j/i E = ( jE/iE)star/( jE/iE)sun − 1, (B.2) μ j/i E = ln(m jE/mi E) m jE/mi E − 1, (B.3) c i E…”
• The Non-carbonaceous–Carbonaceous Meteorite Dichotomy (2020, unknown): “The slope of s-process mixing lines in εiMo–ε94Mo plots can be determined from presolar grain data using the formalism of Dauphas et al. (2004): m = ρ iMo − ρ98Mo · μiMo ρ94Mo − ρ98Mo · μ94Mo where the parameter ρiMo represents the s-process composition relative to the terrestrial Mo isotope…”