Zuffa, G.G. (1987) Unravelling Hinterland and Offshore Palaeogeography from Deep-Water Arenites. In: Legget, J.K. and Zuffa, G.G., Eds., Marine Clastic Sedimentology, Graham & Trotman, London, 39-61.
http://dx.doi.org/10.1007/978-94-009-3241-8_2

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