Materia orgánica y diagénesis de la formación de margas del Mas d´Ascla (Jurásico superior) en la cuenca del Maestrazgo (Cadena Ibérica oriental)
- Permanyer Bastardas, Albert
- Marfil Pérez, Rafaela
- Salas Roig, Ramón
- Peña Blasco, José Andrés de la
- Dorronsoro Fernández, Carlos F.
- Rossi Nieto, Carlos
ISSN: 0213-683X
Año de publicación: 2000
Número: 28
Páginas: 117-120
Tipo: Artículo
Otras publicaciones en: Geogaceta
Resumen
The Mas d'Ascla marls Fm. (Upper Kimmeridgian to lowermost Tithonian) in the Maestrat Basin (Salzedella sub-basin, Castellò de la Plana) displays two organic-carbon-rich horizons which indicate anoxic conditions. The maximum anoxic event is located at the base of the formation corresponding to the lower part of the trangressive system tract. In both horizons the kerogen is mainly of marine origin with algal and amorphous sapropelic organic matter, a low organic carbon content (0.5% - 1.26%) and a low potential yield of hydrocarbons (HC). These data and the Tmax. suggest a mature source-rock which has already generated nearly all HC. Extractable organic matter is fundamentally composed of asphaltenes and resins predominating over saturate and aromatic compounds which have been probably expulsed out of the source rock