Neogene uplift of central eastern Patagonia: Dynamic response to active spreading ridge subduction

Nazca plate (NP); North Taitao Ridge fault (NTRF); South America plate (SAP); Taitao fracture zone (TFZ); Taitao peninsula (TP); Taitao ridge (TR); triangles,

What remains is that (1) the fast rotation of the Hellenides, which must be a consequence of the tear below the eastern Aegean, and the formation of high-temperature domes

One can note that outside our study area, the Amazon Basin displays catchments with very low relief and with areas where deposition occurs, like the northern and southern Amazonian

During his journey on the Beagle, Darwin observed the uniformity in the elevation of coastal Eastern Patagonia along more than 2000 km. More than one century later, the sequences

Tomographic travel- time inversion of seismic data suggests that the crustal structure along the ridge axis is controlled by melt supply; thus, crust is thickest, 8 km, at the

the lacustrine record from Laguna Potrok Aike, southern

Top : side view showing the planar linking complex and the ruffled structure of the copper(II)porphyrin (all meso-aryl groups omitted), bottom: view showing the

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