Hafnium and iron isotopes in early Archean komatiites record a plume-driven convection cycle in the Hadean Earth
Archean (>2.5 billion years) komatiites are considered expressions of mantle plumes that originate from and thereby sample the lowermost mantle overlying the Earth's core. Some komatiites have reported Hf isotope signatures that require a mantle source
|Collections||ANU Research Publications|
|Source:||Earth and Planetary Science Letters|
|01_Nebel_Hafnium_and_iron_isotopes_in_2014.pdf||1.58 MB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.