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The Azuaje travertine: an example of aragonite deposition in a recent volcanic setting, N Gran Canaria Island, Spain



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Rodríguez Berriguete, Álvaro y Alonso-Zarza, Ana María y Cabrera Santana, María del Carmen y Rodríguez González, Alejandro (2012) The Azuaje travertine: an example of aragonite deposition in a recent volcanic setting, N Gran Canaria Island, Spain. Sedimentary Geology, 277-78 . pp. 61-71. ISSN 0037-0738

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URL Oficial: http://www.journals.elsevier.com/sedimentary-geology/‎


The Azuaje travertines in the north of Gran Canary Island crop out in the Azuaje Gorge, which is incised into Miocene
volcanic breccias of the Roque Nublo Formation. This travertine is interesting because of the scarcity of travertines in
the Canary Islands and its close relationship with recent volcanic events. Part of the travertine overlies a lava flow,
dated at 2420±40 years BP. The travertine is composed mainly of aragonite in both perched systems on the
gorge walls and in gorge bottom deposits parallel to the present stream. Perched systems include deposits from
the feeder conduits within the Roque Nublo Formation that spilled out through waterfalls and over barriers. The
gorge (valley) bottom system includes barrier and pool deposits. The main laminated facies are composed mostly
of large fibrous aragonite crystals, while there are also common micritic and porous microfabrics. Shrubs, coated
grains, coated bubbles and rafts are present in many of the deposits. Detailed study of the microfacies shows the
presence of sparsely distributed biogenic features. The δ13C values are between +4.0 and +11.0‰, and the δ18O
values range between −11.0 and −2.0‰ VPDB. These δ13C values lie within the range of those of thermogene
travertines fed by thermal waters that cooled downstream, as indicated by the increase of the carbon and oxygen
isotope values in that direction. The common occurrence of fibrous radial fabrics is interpreted to be due to disequilibrium
conditions during aragonite precipitation. Disequilibrium was likely caused by rapid CO2 degassing of the
thermalwaters that led to a rapid increase in the degree of aragonite saturation. Thus, themorphology of the aragonite
crystals and the isotopic composition indicate that the formation of the Azuaje travertine was mostly due to
abiogenic processes induced by rapid degassing of thermalwaters, linked to the presence of a recent lava flow within
the Gorge. In short, the Azuaje travertine shows the important role of volcanic activity in travertine deposition, in
the facies distribution as well as in the geochemical signatures of the deposits, and so can be used as a recent
analogue for ancient travertine deposits in volcanic settings

Tipo de documento:Artículo
Palabras clave:Travertine, Aragonite, Volcanic settings, CO2 degassing, Canary Islands, Perched systems
Materias:Ciencias > Geología > Mineralogía
Código ID:25233
Depositado:30 Abr 2014 09:24
Última Modificación:30 Abr 2014 12:36

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