Continental topography is dominantly controlled by a combination of crustal thickness and
density variations. Nevertheless, it is clear that some additional topographic component is …

SUMMARY A major challenge in seismic tomography consists in quantifying and
representing model resolution and uncertainty, particularly at global scales. This information …

Rapid plate motion, alongside pronounced variations in age and thickness of the Australian
continental lithosphere, makes it an excellent location to assess the relationship between …

The construction and assessment of model trajectories that link multiple mantle states is
essential to constrain poorly known mantle convection parameters. Previously, volumetric …

We present the first sequential structural restoration with flexural backstrip** of the Gulf of
Mexico US‐Mexico conjugate margin salt basin. We construct four large‐scale (100s of km) …

Mantle convection is a fundamental process in the Earth's system, yet its history remains
poorly known. Sophisticated inverse geodynamic Earth models are available to retrodict …

Reconstructing the thermo-chemical evolution of Earth's mantle and its diverse surface
manifestations is a widely recognised grand challenge for the geosciences. It requires the …

Thick continental lithosphere represents a thermal insulator, promoting less efficient
conductive heat transfer to the surface. As a consequence, the mantle temperature under …

Mantle convection plays a fundamental role in driving evolution of oceanic and continental
lithosphere. In turn it impacts a broad suite of processes operating at or close to Earth's …

Subduction zones are associated with spatially heterogeneous pressure fields that,
depending on location, push/pull on Earth's surface producing dynamic topography (DT) …