Extensional basin evolution in the Cordillera Blanca, Peru: Stratigraphic and isotopic records of detachment faulting and orogenic collapse in the Andean hinterland

Author:

Giovanni Melissa K.1,Horton Brian K.2,Garzione Carmala N.3,McNulty Brendan4,Grove Marty5

Affiliation:

1. Department of Geoscience; University of Calgary; Calgary, Alberta; Canada

2. Institute for Geophysics and Department of Geological Sciences; Jackson School of Geosciences, University of Texas at Austin; Austin; Texas; USA

3. Department of Earth and Environmental Sciences; University of Rochester; Rochester; New York; USA

4. Department of Earth Sciences; California State University Dominguez Hills; Carson; California; USA

5. Department of Geological and Environmental Sciences; Stanford University; Stanford; California; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference97 articles.

1. Structural expression of a rolling hinge in the footwall of the Brenner Line normal fault, eastern Alps;Axen;Tectonics,1995

2. Geological constraints on the kinematics and fault-plane solution of the Quiches fault zone reactivated during the 10 November 1946 Ancash earthquake, northern Peru;Bellier;Bull. Seismol. Soc. Am.,1991

3. Alluvial fans and their natural distinction from rivers based on morphology, hydraulic processes, sedimentary processes, and facies assemblages;Blair;J. Sediment. Res.,1994

4. Climatic and ecologic changes during Miocene surface uplift in the Southern Patagonian Andes;Blisniuk;Earth Planet. Sci. Lett.,2005

5. Bonnot , D. 1984 Neotectonique et tectonique active de la Cordillera Blanca et Callejon de Huaylas (Andes nord-peruviennes) 115 Universite de Paris-Sud Orsay

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