Carbon emissions along divergent plate boundaries modulate icehouse-greenhouse climates
Carbon emissions along divergent plate boundaries modulate icehouse-greenhouse climate transitions through mid-ocean ridge and rift degassing.
Carbon emissions along divergent plate boundaries modulate icehouse-greenhouse climate transitions through mid-ocean ridge and rift degassing.
Using full-waveform seismic tomography to detect craton boundaries and their spatial links to critical metal deposit locations.
Plate tectonic reconstructions and machine learning show that subducting seafloor anomalies promote porphyry copper deposit formation.
Coupling plate tectonic models with thermodynamic carbon outflux estimates to reconstruct solid Earth carbon degassing over the last billion years.
A positive-unlabeled machine learning model predicts spatio-temporal copper prospectivity along the American Cordillera from subduction zone dynamics.
Exceptionally low mid-ocean ridge CO2 outgassing sustained the Sturtian Snowball Earth glaciation for over 50 million years.