Distribución geoquímica y mineralógica del U en el grantio peralumínico de Alburquerque, Cáceres (España)

  1. Reguillón, R.M.
  2. Arribas, A.
  3. Martín Izard, A. 1
  1. 1 Universidad de Oviedo
    info

    Universidad de Oviedo

    Oviedo, España

    ROR https://ror.org/006gksa02

Journal:
Boletín de la Sociedad Española de Mineralogía

ISSN: 0210-6558

Year of publication: 1992

Volume: 15

Issue: 1

Pages: 166-170

Type: Article

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More publications in: Boletín de la Sociedad Española de Mineralogía

Abstract

A study has been carried out on the content and geochemical distrubibution of U in the alkaline and peraluminous granite of Alburquerque. Cáceres, (Spain) and of the primary minerals rich in this element. Of the there petrographic facies distinghed in the study, facies I and facies II are seen to contain the highest mean amounts of uranium. Regarding the mineral phases, uranium is found in uranitita and monacita and also in the intergranular spaces, as demostred by autoradiographic studies.

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