RT Journal Article
T1 Arquitectura estratigráfica de la Fm. Escucha (Albiense) en elflanco sur del Sinclinal de Cueva Foradada. Subcuenca de Oliete(Teruel), Cuenca Ibérica Central
A1 Rodríguez López, Juan Pedro
A1 Meléndez Hevia, Nieves
A1 Soria, Ana Rosa
AB Detailed stratigraphic sections have allowed to establish the stratigraphic architecture of the Escucha Formation in the southern limb of the asymmetrical Cueva Foradada Syncline (Oiete Subbasin, Iberian Basin, Spain). The stratigraphic correlation builded from the studied stratigraphic sections shows the spatial distribution of the main architectural elements and their spatial relationships. Offshore, intertidal, supratidal, flood delta / tidal inlet and bay-lagoon with tidal meandering channel facies associations occurred in a strongly tidal-influenced stratigraphic succession. The occurrence of several key stratigraphic levels characterized by the presence of nodular-iron rich levels with gastropods, levels of oyster accumulations and galuconitic sandstones suggest that the beginning of the Escucha Formation's evolution was characterized by the development of several transgressive periods that interrupted the development of coal-forming and tidal-influenced siliciclastic sedimentary subenvironments.
PB Sociedad Geológica de España.
SN 1576-5172
YR 2005
FD 2005
LK https://hdl.handle.net/20.500.14352/52565
UL https://hdl.handle.net/20.500.14352/52565
LA spa
NO Secretaría de Estado de Educación y Universidades
DS Docta Complutense
RD 8 jul 2024