Palaeogeography and diachronous infill of an ancient deep-marine foreland basin, Upper Cretaceous Cerro Toro Formation, Magallanes Basin

Author:

Bernhardt Anne1,Jobe Zane R.1,Grove Marty1,Lowe Donald R.1

Affiliation:

1. Department of Geological and Environmental Sciences; Stanford University; Stanford; CA; USA

Publisher

Wiley

Subject

Geology

Reference80 articles.

1. The influence of mass transport deposit topography on the evolution of turbidite architecture: the Sierra Contreras, Tres Pasos Formation (Cretaceous), southern Chile;Armitage;J. Sed. Res.,2009

2. Thrust dissection control of deep-water clastic dispersal patterns in the Klematia-Paramythia foreland basin, western Greece;Avramidis;Geol. Mag.,2000

3. Deep-water leveed-channel complexes of the Cerro Toro Formation, Upper Cretaceous, southern Chile;Beaubouef;AAPG Bull,2004

4. Bernhardt , A. Jobe , Z.R. Lowe , D.R. 2008 The evolution of an elongate foreland basin: the deep- to shallow-marine filling of the Cretaceous Magallanes Basin, Chile 268 310

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