Sedimentología de algunas facies de la Formación Coris (Mioceno Medio, Mioceno Superior), Valle Central, Costa Rica, América Central

 

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Detalles Bibliográficos
Autores: Obando, Luis Gmo., Bottazzi, Giovanni, Alvarado, Fernando
Formato: artículo original
Estado:Versión publicada
Fecha de Publicación:2011
Descripción:In the Central Valley of Costa Rica exists a principal sandy- quartz sequence (Middle Miocene to Upper Miocene). Occasionally this rocks are inter-bedded with coal seams (lignite 0.3 to 1 m thick) and silstones very riches in organic matter. The new data and reinterpretation of the sequences, permitted defined the sedimentary facies: Silicoclastic Platform (mixed facies), Open Bay Facies, Bar Facies (bar front (middle shoreface) and upper shoreface). Those facies represent a Strand Plain, generated by Miocene inter-ceanic currents, through the channel genetic related with the Sinistral Costa Rica Transcurrent Fault System. That fault,  has segmented the national territory and generated the pull-apart Basin in the Central Valley. The rapidly susidence accumulated thick shallow deposits. 
País:Portal de Revistas UCR
Institución:Universidad de Costa Rica
Repositorio:Portal de Revistas UCR
Lenguaje:Español
OAI Identifier:oai:portal.ucr.ac.cr:article/13075
Acceso en línea:https://revistas.ucr.ac.cr/index.php/geologica/article/view/13075