The events and processes associated with the meeting of oceanic plateaus and subduction
zones have significant implications for our understanding of lithospheric strength, structure …

Allochthonous accreted terranes are exotic geologic units that originated from anomalous
crustal regions on a subducting oceanic plate and were transferred to the overriding plate by …

The Chilean margin is one of the Earth's tectonically most active plate boundaries, and yet,
some of its segments are still underexplored. Here, we present amphibious data from the …

Abstract The Piton de la Fournaise basaltic volcano, on La Réunion Island in the western
Indian Ocean, is one of the most active volcanoes in the world. This volcano is classically …

Since marine seismic studies are relatively sparse and unevenly distributed, detailed
tomographic images of the Moho geometry under large parts of the world's oceans and …

Broadband seismograms from the EarthScope Transportable Array and Superior Province
Rifting EarthScope Experiment (SPREE) deployments are used to map the crust and …

Seafloor spreading can be explained by different dynamic mechanisms, magmatically or
tectonically dominated. The Southwest Sub‐basin, located at the southwest tip of the …

The Réunion mantle plume has shaped a large area of the Earth's surface over the past 65
million years: from the Deccan Traps in India along the hotspot track comprising the island …

We infer the lithospheric structure beneath the Hawaiian Swell based on a joint inversion of
ambient noise and teleseismic Rayleigh waves collected during the PLUME experiment …

Crustal structure preserves a unique record of physical and chemical conditions of its
formation and later modification by geodynamic processes. The existence of broad global …