The metamorphic rocks of the Nunatak Viedma in the Southern Patagonian Andes: Provenance sources and implications for the early Mesozoic Patagonia-Antarctic Peninsula connection

Author:

Suárez Rodrigo J.,Ghiglione Matías C.,Calderón Mauricio,Sue Christian,Martinod Joseph,Guillaume Benjamin,Rojo DiegoORCID

Funder

projects Agencia

CONICET

Argentinian-French ECOS-SUD project

Proyecto FONDECYT

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference156 articles.

1. A 100-m.y.-long window onto mass-flow processes in the Patagonian Mesozoic subduction zone (Diego de Almagro Island, Chile);Angiboust;The Geological Society of America,2018

2. Hot subduction in the middle Jurassic and partial melting of oceanic crust in Chilean Patagonia;Angiboust;Gondwana Res.,2017

3. Active or passive continental margin? Geochemical and Nd isotope constraints of metasediments in the backstop of a pre-Andean accretionary wedge in southernmost Chile (46°30’ – 48°30’S);Augustsson,2003

4. Cathodoluminescence spectra of detrital quartz as provenance indicators for Paleozoic metasediments in southern Andean Patagonia;Augustsson;J. S. Am. Earth Sci.,2003

5. Provenance of late Palaeozoic metasediments of the Patagonian proto-Pacific margin (southernmost Chile and Argentina);Augustsson;Int. J. Earth Sci.,2008

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