Article citationsMore>>

Rodriguez Alonso, M.D., Diez Belda, M.A., Perejon, A., Pieren, A., Linan, E., Lopez Diaz, F., Moreno, F., Gamez Vintaned, J.A., Gonzalez Lodeiro, F., Martinez Poyatos, D. and Vegas, R. (2004) Dominio del Complejo Esquisto-Grauvaquico. Estratigrafia. La secuencia litoestratigrafica del Neoproterozoico—Cambrico Inferior. In: Vera, J.A., Ed., Geologia de Espana, Sociedad Geologica de Espana—Instituto Geologico y Minero de Espana, Madrid, 78-81.

has been cited by the following article:

• TITLE: Transport-Limited Denudation Regime Inferred from Sand Petrography and Chemical Composition: Cenozoic Sediments from the Guadiana Basin (SW Spain)

  AUTHORS: José Arribas, Meaza Tsige, Guillermina Garzón, Rosa Tejero

  KEYWORDS: Provenance, Geochemistry, Sediment Composition, Intraplate Basins, Denudation Regimes

  JOURNAL NAME: International Journal of Geosciences, Vol.5 No.5, April 29, 2014

  ABSTRACT: The Guadiana Basin is an E-W intraplate Cenozoic basin located in SW of the Iberian Peninsula, covering an area close to 6000 km2. NE-SW Alpine faults divide the basin into two subbasins: the Vegas Altas (VA) to the East, and the Vegas Bajas (VB) to the West. Sedimentary record consists of