Nuevos datos geológicos sobre las mineralizaciones de grafito de la Banda Metamórfica de Aracena, Huelva (Macizo Ibérico Meridional).

  1. C. Fernández Rodríguez 1
  2. J. C. Fernández Caliani 1
  3. A. Miras 2
  4. J. F. Barrenechea 3
  5. F. J. Luque 3
  6. M. Rodas 3
  1. 1 Dpto.Geología, Fac. CC. Experimentales, Univ. Huelva, 21819-Huelva.
  2. 2 Dpto.Cristalografía, Mineralogía y Química Agrícola, Fac. Química, Univ. Sevilla, 41071-Sevilla.
  3. 3 Dpto. Cristalografía y Mineralogía, Fac. Geología, Univ. Complutense, 28040-Madrid.
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Journal:
Geogaceta

ISSN: 0213-683X

Year of publication: 1996

Issue: 20

Pages: 1576-1577

Type: Article

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Sustainable development goals

Abstract

In this work a detailed geological map of the graphite mineralizations of the Aracena Metamorphic Belt (SW Iberian Massif) is shown. Three types of mineralizations have been distinguished according to lithostratigraphic and structural criteria: 1) Stratiform deposits related to gneissic lenticular bodies embedded within a complex calc-silicate sequence 2) Veinlets of graphite cutting across mafic granulites; and 3) Disseminated graphite within gneisses and quartzites belonging to the Fuente del Oro series. Only the first type of mineralizations could have an economic interest.

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