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.
ben-mather
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Craton boundary detection from full-waveform tomography model reveals links to critical metal deposits
Using full-waveform seismic tomography to detect craton boundaries and their spatial links to critical metal deposit locations.
hojat-shirmard
Regional carbonate compensation depth variability in the Pacific Ocean since the Oligocene
Reconstructing regional carbonate compensation depth variability in the Pacific Ocean since the Oligocene to understand deep-sea carbon cycling.
faranak-dalvand
Subducting seafloor anomalies promote porphyry copper formation
Plate tectonic reconstructions and machine learning show that subducting seafloor anomalies promote porphyry copper deposit formation.
ben-mather
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
Spreading ridge migration enabled by plume-ridge de-anchoring
Numerical modelling shows that high-buoyancy mantle plumes can capture and de-anchor spreading ridges, enabling their migration over vast distances.
ben-mather
Spatio-temporal copper prospectivity in the American Cordillera predicted by positive-unlabeled machine learning
A positive-unlabeled machine learning model predicts spatio-temporal copper prospectivity along the American Cordillera from subduction zone dynamics.
christopher-p.-alfonso
Duration of Sturtian 'Snowball Earth' glaciation linked to exceptionally low mid-ocean ridge outgassing
Exceptionally low mid-ocean ridge CO2 outgassing sustained the Sturtian Snowball Earth glaciation for over 50 million years.
adriana-dutkiewicz
Flexural isostatic response of continental-scale deltas to climatically driven sea level changes
Simulating how flexural isostatic responses to climatically driven sea level changes shape continental-scale delta evolution on passive margins.
sara-polanco
Determining subsurface temperature & lithospheric structure from joint geophysical-petrological inversion: A case study from Ireland
A joint geophysical-petrological inversion combining seismic surface-wave data with thermodynamic modelling to map subsurface temperature in Ireland.
emma-l.-chambers