dc.contributor
Balduin, Alexander
dc.contributor
Noack, Lena
dc.date.accessioned
2023-05-23T15:19:53Z
dc.date.available
2023-05-23T15:19:53Z
dc.identifier
https://doi.org/10.35003/5TTOZG
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/39432
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-39149
dc.description
• Stagnant lid C-O-H outgassing rates predicted across mantle oxidation states.
• Fully-coupled convection model reveals limiting effect of mantle volatile budget.
• Early Archean CO2 outgassing was not necessarily stronger than the modern rate.
dc.subject
Computer and Information Science
dc.subject
Secondary atmospheres
dc.subject
Planetary dynamics
dc.subject
Mantle convection
dc.subject
Numerical modelling
dc.title
Replication Data for: Low volcanic outgassing rates for a stagnant lid Archean earth with graphite-saturated magmas
dcterms.accessRights.openaire
metadata only access
