Contribución al conocimiento paleontológico, geocronológico y paleoambiental de la Formación Jackson inferior (Eoceno Superior), en la Cuenca de Burgos, Tamaulipas, México
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La Cuenca de Burgos en el noreste de México tiene escasa información geológica publicada. Datos de superficie se conocen por publicaciones diversas esporádicas y cartas geológico-mineras a escalas 1:250,000 y 50,000 elaboradas por el Servicio Geológico Mexicano, los afloramientos en esta región son dispersos y su dimensión es limitada. La información de subsuelo es restringida y se conoce por aportes que Petróleos Mexicanos ha permitido divulgar. La estratigrafía, modelos sedimentarios y estructurales de esta cuenca, son extrapolados de Texas, o bien, son pocos los estudios estratigráficos y sedimentológicos que sirven como referencia análoga para inferir modelos de sedimentación aplicables a la exploración de carbón, uranio, acuíferos y yacimientos de gas en el subsuelo o con fines académicos. Por primera vez en la Cuenca de Burgos se utilizan isótopos 87Sr/86Sr para obtener una edad geocronológica de 36.75 (+2.65/-2.05) Ma, para la Formación Jackson inferior. Este intervalo estratigráfico tiene el ostréido Crassostrea cf. alabamiensis reportado por primera vez en esta cuenca; a partir de la concha bien preservada de este molusco, se obtuvo la muestra para los análisis de Sr. Los datos estratigráficos y paleontológicos de la sección estudiada sugieren interpretar una sucesión de subambientes de barra, laguna y planicie fluvio-lacustre para una costa litoral, dominada por olas y mareas, en un episodio transgresivo (transgressive system tract), cuya edad se incluye en el piso Priaboniano (Eoceno Superior).
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