Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/16876
Title: Coastal salina evaporites of the Triassic-Liassic boundary in the Iberian Peninsula: the Alacón borehole
Author: Ortí Cabo, Federico
Salvany, Josep Maria
Keywords: Evaporites
Salines
Triàsic
Serralada Ibèrica
Evaporites
Salines
Triassic Period
Iberian Mountains (Spain)
Issue Date: 2004
Publisher: Universitat de Barcelona (UB). Institut de Ciències de la Terra Jaume Almera (ICTJA). Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDEA). Universitat Autonònoma de Barcelona (UAB). Consejo Superior de Investigaciones Científicas (CSIC)
Abstract: The evaporite unit (the Lécera Formation), which was formed at the Triassic¿Liassic boundary in the Aragonian Branch of the Iberian Chain, was studied at the 01 Alacón borehole (Alacón village, Teruel province), where it is mainly constituted by a thick (>e and reflect deeper water settings, whereas in the upper part they correspond to shallower water settings. The evaporite sedimentation mainly occurred in a subsiding coastal basin of the salina or lagoon type. In this setting, the subaqueous precipitation of the carbonate and gypsum lithofacies was followed, in each cycle, by the interstitial growth of anhydrite in exposed conditions. As a whole, the evaporite succession reflects an infilling process. The conversion into anhydrite of the selenitic gypsum -probably also of the rest of depositional gypsum lithofaciesstarted under synsedimentary conditions and followed during shallow to moderate burial diagenesis.
Note: Reproducció del document publicat a http://www.geologica-acta.com/pdf/vol0204a05.pdf
It is part of: Geologica Acta, 2004, vol. 2, núm. 4, p. 291-304
URI: http://hdl.handle.net/2445/16876
ISSN: 1695-6133
Appears in Collections:Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)

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