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: Artículo publishedVersion
Publicado: 2007
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
https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v62_n2_p_Palma_oai
Aporte de:
Repositorio Digital de la Universidad de Buenos Aires (UBA) de Universidad de Buenos Aires

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