CARBONATOS RESERVATÓRIO DA FORMAÇÃO MACAÉ, BACIA DE CAMPOS, RJ, BRASIL PARTE I - CONTRIBUIÇÃO À GEOQUÍMICA DOS CARBONATOS
Abstract
A Formação Macaé, objeto deste estudo, representa o episódio de Margem Continental Aberta, fase de mar estreito, da evolução tectono-sedimentar da Plataforma Brasileira.Os valores de elementos químicos menores, traço e isotópicos apresentados na análise de rocha total são similares aos apresentados por sedimentos originados em plataformas marinhas rasas. Ambiente restrito com salinidade elevada fica demonstrado pela baixa diversidade de foraminíferos e valores elevados de álcalis e cloro em rocha total. Conteúdo de 8C13 ao redor de +4 reforça esta idéia.
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