A joint geophysical-petrological inversion combining seismic surface-wave data with thermodynamic modelling to map subsurface temperature in Ireland.
The temperature distribution in the crust, and associated uncertainty, was simulated from the ensemble of Curie depth realisations assigned to a lower thermal boundary condition of …
A 3D temperature model of Ireland has provided a unique insight into the thermochemical structure within Ireland's subsurface.
Heat‐producing elements have been more successfully reworked into the upper crust of Laurentia than Avalonia during continental accretion.