Constraints on the origin of Os-isotope disequilibrium in included and interstitial sulfides in mantle peridotites: Implications for the interpretation of Os-isotope signatures in MORB and Abyssal Peridotites

John C Lassiter, University of Texas at Austin, Department of Earth and Planetary Sciences, Austin, United States
Back to: Heterogeneity in Earth's Deep Interior: From Natural and Laboratory Observations to Theoretical Models III