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The Tremp Formation is the continental lateral equivalent of the Ar&#233;n Sandstone Formation. Both formations are part of regressive depositional sequences, formed during a relative sea level rise.  At the top of the Isona anticline and in tbe south flank of the Sant Comeli anticline, four lithostratigraphic units are distinguisbed in the Tremp Formation. The sedimentary evolution of each of these units is related to tectonic reactivation and a slow down of the diastrophism. The successive sedimentary environments inferred for these units are the following: lagoon and/or fluvial plain, fluvial plain, tidal flat and/or lacustrine-palustrine. At the base and/or within sorne of these units there are progressive unconformities. The maximum slow down of the diastrophism would correspond to sedimentation in the tidal flat and/or lacustrine environments.  La Fm. Tremp es el equivalente lateral continental de la Fm. Arenisca de Ar&#233;n. Ambas formaciones forman parte de secuencias deposicionales de car&#225;cter regresivo, en r&#233;gimen de subida relativa del nivel del mar.  En el cierre peridinal del anticlinal de Isona y en el flanco S del anticlinal de Sant Comeli, dentro de la Fm. Tremp, se identifican cuatro unidades estratigr&#225;ficas cuya evoluci&#243;n sedimentaria estuvo ligada a reactivaciones tect&#243;nicas y a la desaceleraci&#243;n del diastrofismo. Los sucesivos ambientes de sedimentaci&#243;n que se infieren en sentido vertical para estas unidades son: ambientes de &#194;&#171;lagoon&#194;&#187; y/o llanura fluvial, llanura fluvial, llanura de marea y/o lacustrepalustre. En la base y/o en el interior de algunas de estas unidades existen discordancias progresivas, la desaceleraci&#243;n m&#225;xima del diastrofismo se corresponder&#237;a con la sedimentaci&#243;n en ambientes de llanura de marea y/o lacustre

Sedimentación sinectónica asociada a una subida relativa del nivel del mar durante el Cretácico superior (Fm. Tremp, provincia de Lérida)