The detrital record of late-Miocene to Pliocene surface uplift and exhumation of the Venezuelan Andes in the Maracaibo and Barinas foreland basins

Author:

Bermúdez M. A.12,Hoorn C.3,Bernet M.2,Carrillo E.4,van der Beek P. A.2,Garver J. I.5,Mora J. L.1,Mehrkian K.2

Affiliation:

1. Escuela de Geología; Minas y Geofísica; Facultad de Ingeniería; Universidad Central de Venezuela; Caracas Venezuela

2. Institut des Science de la Terre; Université Joseph Fourier; Grenoble France

3. Institute for Biodiversity and Ecosystem Dynamics (IBED); University of Amsterdam; Amsterdam The Netherlands

4. Instituto de Ciencias de la Tierra; Facultad de Ciencias; Universidad Central de Venezuela; Caracas Venezuela

5. Geology Department; Union College; Schenectady NY USA

Funder

Consejo de Desarrollo Científico y Humanístico, Universidad Central de Venezuela

de la Universidad Central de Venezuela (UCV)

Fondo Nacional de Ciencia Tecnología e Innovación

Petróleos de Venezuela

Publisher

Wiley

Subject

Geology

Reference86 articles.

1. Structure of the Merida Andes, Venezuela: relations with the South America-Caribbean geodynamic interaction;Audemard;Tectonophysics,2002

2. Final closure of Panama and onset of nothern hemisphere galciation;Bartoli;Earth Planet. Sci. Lett.,2005

3. Baudin , F. Tribovillard , N. Trichet , J. 2007 Géologie de la Matière Organique, Edition Vuibert, Paris, Collection Interactions 263

4. An integrated analysis of an orogen-sedimentary basin pair: latest Cretaceous-Cenozoic evolution of the linked Eastern Cordillera orogen and the Llanos foreland basin of Colombia;Bayona;Geol. Soc. Am. Bull.,2008

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