dc.contributor
Kleine, Thorsten
dc.creator
Kleine, Thorsten
dc.date.accessioned
2023-05-23T15:19:53Z
dc.date.available
2023-05-23T15:19:53Z
dc.identifier
https://doi.org/10.35003/5N1IU8
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/39431
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-39148
dc.description
• The Mo-Ru correlation only exists for non-carbonaceous meteorites.
• Earth's mantle falls off the Mo-Ru correlation.
• The Mo-Ru isotope systematics are consistent with heterogeneous accretion of Earth.
dc.subject
Earth and Environmental Sciences
dc.subject
Late stage accretion
dc.subject
Siderophile elements
dc.subject
Isotope dichotomy
dc.title
Replication Data for: Heterogeneous accretion of Earth inferred from Mo-Ru isotope systematics
dcterms.accessRights.openaire
metadata only access
