Seismic travel-time tomography of the mantle under SE Asia reveals patterns of subduction-
related seismic P-wave velocity anomalies that are of great value in hel** to understand …

The Mediterranean offers a unique opportunity to study the driving forces of tectonic
deformation within a complex mobile belt. Lithospheric dynamics are affected by slab …

Abstract Formation of the Tibetan Plateau is generally ascribed to the Cenozoic India–Asia
collision. However, the origin of along-strike deformation of the Indian mantle lithosphere …

Sustainable development and the transition to a clean-energy economy drives ever-
increasing demand for base metals, substantially outstrip** the discovery rate of new …

We present a new global thermochemical model of the lithosphere and underlying upper
mantle constrained by state of the art seismic waveform inversion, satellite gravity (geoid …

We study the upper mantle P wave velocity structure below the Euro‐Mediterranean area,
down to 1000 km depth, by seismic travel time tomography. We invert summary residuals …

Mechanisms for uplift and deformation of the Tibetan Plateau remain vigorously debated;
hypotheses include stepwise growth, distributed thickening, and crustal channel flow, each …

The evolution of the European Cenozoic Rift System (ECRIS) and the Alpine orogen is
discussed on the base of a set of palaeotectonic maps and two retro-deformed lithospheric …

Constraints on mantle temperatures are fundamental for a better understanding of the
dynamics of the Earth. We evaluate how well upper-mantle thermal structure can be inferred …

Unlike in the ocean basins where the shallow mantle eventually contributes to the
destruction of the overlying crust, the shallow mantle beneath continents serves as a stiff …