Chronology of deposition and unconformity development across the Cretaceous–Paleogene boundary, Magallanes-Austral Basin, Patagonian Andes

Author:

George Sarah W.M.,Davis Sarah N.,Fernández Roy A.,Manríquez Leslie M.E.,Leppe Marcelo A.,Horton Brian K.,Clarke Julia A.

Funder

Fondo Nacional de Desarrollo Científico y Tecnológico

National Science Foundation

Comisión Nacional de Investigación Científica y Tecnológica

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference163 articles.

1. The Cretaceous-Tertiary boundary in southern low-latitude regions: preliminary study in Pernambuco, northeastern Brazil;Albertão;Terra. Nova,1994

2. Thermal history of the Maastrichtian-Eocene Magallanes (Austral) foreland basin, Patagonia (50.5-51.5°S): preliminary findings from vitrinite reflectance analysis and detrital zircon thermochronology: AAPG Eastern Section Meeting, Indianapolis;Ali;Indiana,2015

3. Paleogene tectonic and thermal evolution of the Magallanes Basin, Chile, 50°30’-51°30’S: A study using zircon (U-Th)/He thermochronology and vitrinite reflectance;Ali,2016

4. Geometry and evolution of the frontal part of the Magallanes foreland thrust and fold belt (Vicuña area), Tierra del Fuego, southern Chile;Alvarez-Marrón;Am. Assoc. Pet. Geol. Bull.,1993

5. The Farallon-Aluk ridge collision with South America: implications for the geochemical changes of slab window magmas from fore-to back-arc;Aragón;Geosci. Front,2013

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