Subtropical carbonates from the Callovian Calabozo Formation, and their diagenesis, Neuquen Basin, Mendoza province

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Detailed study of Callovian carbonates of the Calabozo Formation (30 m) in western Argentina, reveals the abundance of benthic carbonates particles produced by organisms that are light dependent, and non-skeletal grains such as ooids and peloids. The biota consists of bivalves, dasyclads (Salpingopo...

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Detalles Bibliográficos
Autores principales:	Palma, R.M., Mehdli, M., Bressan, G.S., Kietzmann, D.A.
Formato:	JOUR
Materias:	Carbonate ramp Diagenesis Jurassic Microfacies Photozoan Association biota bivalve Callovian carbonate ramp cement diagenesis echinoderm gastropod microfacies paleoenvironment petrography subtropical region Argentina Neuquen Basin South America Anthozoa Bivalvia Bryozoa Cyanobacteria Cylindroporella Echinodermata Foraminifera Gastropoda Ostracoda Rivularia (cyanobacterium) Scleractinia
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00044822_v62_n2_p_Palma
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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