Global Hydrogen Production During High-Pressure Serpentinization of Subducting Slabs
Quantifying global hydrogen production from high-pressure serpentinisation of subducting slabs over the last 5 million years.
andrew-s.-merdith
•
•
1 min read
Kimberlite eruptions driven by slab flux and subduction angle
Machine learning reveals that the volume and angle of subducted oceanic plates control where and when diamond-bearing kimberlite eruptions occur.
ben-mather
Deep time spatio-temporal data analysis using pyGPlates with PlateTectonicTools and GPlately
GPlately: a Python interface for deep-time spatio-temporal data analysis using pyGPlates, simplifying plate tectonic reconstructions.
ben-mather
The isotopic origin of Lord Howe Island reveals secondary mantle plume twinning in the Tasman Sea
First radiogenic isotope data from Lord Howe Island lavas reveal a secondary mantle plume twin in the Tasman Sea with a distinct deep mantle source.
angus-rogers
Anomalously High Heat Flow Regions Beneath the Transantarctic Mountains and Wilkes Subglacial Basin in East Antarctica Inferred From Curie Depth
Curie depth estimates from airborne magnetic data reveal anomalously high geothermal heat flow beneath the Transantarctic Mountains and Wilkes Subglacial Basin.
maximilian-lowe
Iron isotope systematics during igneous differentiation in lavas from Kīlauea and Mauna Loa, Hawai'i
Iron isotope and hafnium data from Kīlauea and Mauna Loa lavas reveal how igneous differentiation and mantle source heterogeneity shape Hawaiian volcanism.
saskia-ruttor
Evolution of Earth’s tectonic carbon conveyor belt
Reconstructing the oceanic carbon conveyor belt over 250 million years reveals plate tectonics as a pivotal driver of Mesozoic climate change.
dietmar-muller
Constraining the response of continental-scale groundwater flow to climate change
A scalable numerical framework for continental groundwater flow modelling, constrained by hydraulic head, recharge, and borehole temperature data using Bayesian inversion.
ben-mather
Intraplate volcanism triggered by bursts in slab flux
Modelling 100 million years of subducted slab volume reveals that bursts in slab flux trigger intraplate volcanism in eastern Australia.
ben-mather
An Early Cretaceous subduction-modified mantle underneath the ultraslow spreading Gakkel Ridge, Arctic Ocean
Seafloor lavas from the ultraslow Gakkel Ridge preserve geochemical signatures of an Early Cretaceous subduction zone, revealing ancient mantle heterogeneity beneath the Arctic …
marianne-richter