This study provides an integrated review of plate tectonic models of the evolution of the
Antarctica–Patagonia connection compared to geological records collected on land in …

A vast ocean basin has spanned the region between the Americas, Asia and Australasia for
well over 100 Myr, represented today by the Pacific Ocean. Its evolution includes a number …

A complete circum-Antarctic seaway did not open until both the South Tasman Rise cleared
the Oates Land coast of East Antarctica and Drake Passage opened between the southern …

We estimate the upper mantle temperature of the Antarctic Plate based on the thermoelastic
properties of mantle minerals and S velocities using a new 3‐D shear velocity model, AN1 …

We present a tectonic interpretation of the breakup and early seafloor spreading between
India and Antarctica based on improved coverage of potential field and seismic data off the …

The Patagonian slab window is a subsurface tectonic feature resulting from subduction of
the Nazca–Antarctic spreading-ridge system (Chile Rise) beneath southern South America …

Precise relative sea level (RSL) data are important for inferring regional ice sheet histories,
as well as helping to validate numerical models of ice sheet evolution and glacial isostatic …

P wave velocity models were obtained by forward and inverse modeling from 38 ocean
bottom seismometers deployed in the central East subbasin of the South China Sea (SCS) …

After isostatic correction for their sedimentary fill, the depths of two small oceanic basins in
the southern Scotia Sea suggest that both started to open in mid to late Eocene times …

Ona Basin is a small intra-oceanic basin located in the southwestern corner of the Scotia
Sea. This region is crucial for an understanding of the early phases of opening of Drake …