Solid Earth Carbon Degassing and Sequestration Since 1 Billion Years Ago
Coupling plate tectonic models with thermodynamic carbon outflux estimates to reconstruct solid Earth carbon degassing over the last billion years.
r.-dietmar-muller
Coupling plate tectonic models with thermodynamic carbon outflux estimates to reconstruct solid Earth carbon degassing over the last billion years.
Exceptionally low mid-ocean ridge CO2 outgassing sustained the Sturtian Snowball Earth glaciation for over 50 million years.
Quantifying global hydrogen production from high-pressure serpentinisation of subducting slabs over the last 5 million years.