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Nesbitt, H.W., Fedo, C.M. and Young, G.M. (1997) Quartz and Feldspar Stability, Steady and Non-Steady-State Weathering, and Petrogenesis of Siliciclastic Sands and Muds. Journal of Geology, 105, 173-191.

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