Along-strike variability of back-arc basin collapse and the initiation of sedimentation in the Magallanes foreland basin, southernmost Andes (53-54.5°S)

Author:

McAtamney Janelle1,Klepeis Keith1,Mehrtens Charlotte1,Thomson Stuart2,Betka Paul3,Rojas Lisandro4,Snyder Shane1

Affiliation:

1. Department of Geology; University of Vermont; Burlington; Vermont; USA

2. Department of Geosciences; University of Arizona; Tucson; Arizona; USA

3. Jackson School of Geosciences; University of Texas at Austin; Austin; Texas; USA

4. Enap-Sipetrol; Santiago; Chile

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference88 articles.

1. Modified Gulf of California model for South Georgia, north Scotia Ridge, and implications for the Rocas Verdes back-arc basin, southern Andes;Alabaster;Geology,1990

2. Allen , R. B. 1982 Geología de la Cordillera Sarmiento, Andes Patagónicos, Entre los 51°00′ y 52°15′ Lat. S, Magallanes, Chile Bol. Serv. Nac. Geol. Mineria 38 Serv. Nac. de Geol. y Minería Chile Santiago

3. Geometry and evolution of the frontal part of the Magallanes foreland thrust and fold belt (Vicuña Area), Tierra del Fuego, southern Chile;Alvarez-Marrón;AAPG Bull.,1993

4. Facies, architecture and origin of a reservoir-scale sand-rich succession within submarine canyon fill: Insights from Wagon Caves rock (Paleocene) Santa Lucia Range, California, U.S.A.;Anderson;J. Sediment. Res.,2006

5. Detrital-zircon geochronology of the eastern Magallanes foreland basin: Implications for Eocene kinematics of the northern Scotia Arc and Drake Passage;Barbeau;Earth Planet. Sci. Lett.,2009

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