dc.contributor
Balduin, Alexander
dc.creator
Gregory J., Archer
dc.creator
Emily A. Worsham
dc.creator
Andreas, Stracke
dc.creator
Matthew G., Jackson
dc.creator
Thorsten Kleine,
dc.date.accessioned
2023-05-23T15:21:22Z
dc.date.available
2023-05-23T15:21:22Z
dc.identifier
https://doi.org/10.35003/YCUKOX
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/39503
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-39221
dc.description
• 182W deficits in ocean island basalts are confirmed using a
new method
• Correlated 182W-183W anomalies that are present in prior datasets are not
confirmed, ruling out a nucleosynthetic origin for 182W deficits
• 182W deficits may reflect either core-mantle interaction or an
overabundance of late-accreted materials
• Mo isotope data do not reveal resolved nucleosynthetic anomalies
• Combined W-Mo data rule out significant contribution of CC-like material to Earth’s core or late accretion
dc.subject
Earth and Environmental Sciences
dc.title
Replication Data for: Origin of 182W anomalies in ocean island basalts
dcterms.accessRights.openaire
metadata only access
