Abstract The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐ enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …
Global deep‐time plate motion models have traditionally followed a classical rigid plate approach, even though plate deformation is known to be significant. Here we present a …
During evolution of the South Sandwich subduction zone, which has consumed South American Plate oceanic lithosphere, somehow continental crust of both the South American …
G Eagles, W Jokat - Tectonophysics, 2014 - Elsevier
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 …
Abstract The South Atlantic region displays (1) a topographic gradient across the basin, with Africa elevated relative to South America,(2) a bimodal spreading history with fast spreading …
Subduction zones and their associated slabs are the main drivers of plate tectonics and mantle flow, but how these zones initiate remains enigmatic. In the Scotia Sea region …
Abstract The Scotia Sea is one of the tectonically most complex and least understood back- arc basins on Earth, which partly results from its remote location making the acquisition of …
Mixed (turbidite-contourite) depositional systems are formed by a complex interplay of deep- water processes. An evaluation of their morphological elements and their lateral and spatial …
YM Martos, M Catalán… - Journal of Geophysical …, 2019 - Wiley Online Library
The sinking of the ocean sea bottom is produced by thermal cooling of the lithosphere. This evolution is determined by the underlying asthenospheric mantle. Estimation of the Curie …