Microbial-dominated carbonate platforms during the Ladinian rifting: sequence stratigraphy and evolution of accommodation in a fault-controlled setting (Catalan Coastal Ranges, NE Spain)

Author:

Mercedes-Martín R.1,Salas R.1,Arenas C.2

Affiliation:

1. Departament de Geoquímica; Petrologia i Prospecció Geològica; Facultat de Geologia; Universitat de Barcelona; C/Martí i Franquès s/n Barcelona 08028 Spain

2. Departamento de Ciencias de la Tierra; Área de Estratigrafía; Universidad de Zaragoza; C/Pedro Cerbuna, 12 Zaragoza 50009 Spain

Publisher

Wiley

Subject

Geology

Reference112 articles.

1. The carbonate ramp - an alternative to the shelf model;Ahr;Trans. Gulf Coast Assoc. Geol. Soc.,1973

2. Classification and environmental significance of crytalgal limestones and dolomites, with illustrations from the Cambrian and Ordovician of south western Alberta;Aitken;J. Sed. Petrol.,1967

3. Growth morphologies of modern marine stromatolites: a case study from Highborne Cay, Bahamas;Andres;Sed. Geol.,2006

4. The epeiric carbonate platform (Imón and Isábena Formations) of the Upper Triassic from the Northeastern Iberian Peninsula;Arnal;Acta Geol. Hisp.,2002

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