Geology of Almería – semi-desert zone of Spain

Autor

  • Małgorzata Labus Wydział Górnictwa i Geologii, Politechnika Śląska

DOI:

https://doi.org/10.7494/geotour.2009.16-17.33

Słowa kluczowe:

Almeria, Rodalquilar, Cabo de Gata, bentonite, gold

Abstrakt

The paper presents selected geosites in the arid Province of Almería (Andalucia, Spain). This region is famous of exceptional, climatic and environmental conditions as well as of geological features. The three geological units are distinguishable in the Almeria: strongly folded and deformed metamorphic rocks of the Iberian Massif, Alpine mountain chain of the Betic Cordilliera and intra-montane basin filled with Neogene sediments. The most interesting is the region of Cabo de Gata-Nijar Natural Park, where the Miocene volcanic domes and calderas can be seen in the field. There is also a variety of exposed, igneous and sedimentary rock, as well as the relics of gold mine in Rodalquilar.

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Bibliografia

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Sänger von Oepen, P., Friedrich, G., Vogt, J.H., 1989. Fluid evolution, wallrock alteration, and ore mineralization associated with the Rodalquilar epithermal gold-deposit in southeast Spain. Mineralium Deposita, 24: 235-243.

Toscani, L., Venturelli, G., Barbieri, M., Capedri, S., Fernandez Soler, J. M., Oddone M., 1990. Geochemistry and petrogenesis of two-Pyroxene andesites from Sierra de Gata (SE Spain). Mineralogy and Petrology, 41: 199-213.

Villalobos Megia, M. (red.), 2003. Geology of the Arid Zone of Almeria, South East Spain, An educational field guide, State water Company for the Southern Basin S.A. (ACUSUR).

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Opublikowane

2018-03-07

Jak cytować

Labus, M. (2018). Geology of Almería – semi-desert zone of Spain. GEOTOURISM (Geoturystyka), (16-17), 33. https://doi.org/10.7494/geotour.2009.16-17.33

Numer

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