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Gromet, L.P., Dymek, R.F., Haskin, L.A. and Korotev, R.L. (1984) The North American Shale Composite: Its Composition, Major and Trace Element Characteristics. Geochimica et Cosmochimica Acta, 48, 2469-2482.
http://dx.doi.org/10.1016/0016-7037(84)90298-9

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