The Scotia Sea and surrounding Scotia Arc have evolved over the past 40 Ma, by extension
behind an east-migrating subduction zone, at the boundary between the South American …

A minimum-complexity tectonic reconstruction, based on published and new basin opening
models, depicts how the Scotia Sea grew by Cenozoic plate divergence, dismembering a …

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 …

Source parameter inversion of P and SH waveforms and amplitudes for 20 shallow
earthquakes using a singular value decomposition technique provides important constraints …

Three types of glaucony grains were identified in the late Eocene (~ 35.5–34.1 Ma)
sediments from Ocean Drilling Program (ODP) Hole 696B in the northwestern Weddell Sea …

Glauconite must be assessed as mica-rich mica-smectite R3 interstratified mineral, with the
pure end-member mica also having intrinsic K-deficient chemical characteristics (K+~ 0.8 …

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 …

Joint inversion of isochron and flow line data from the flanks of the extinct West Scotia Ridge
spreading center yields five reconstruction rotations for times between the inception of …

Ten years after the USAC (US–Argentina–Chile) Project, which was the most
comprehensive aeromagnetic effort in the Antarctic Peninsula and surrounding ocean …

The opening of Powell Basin was part of the regional response to N55° W relative plate
motion of South America away from Antarctica, which led to the formation of Drake Passage …