RT Journal Article
T1 Caracterización de la unidad Conglomerados de Valdemeca en la transición Pérmico-Triásico de la Cordillera Ibérica centro- oriental.
A1 De la Horra, R.
A1 López Gómez, José
A1 Arche, Alfredo
AB The Valdemeca Conglomerates unit is here described as the basal part of the Late Permian-Early Triassic sedimentary cycle in the central-eastern part of the Iberian Ranges, equivalent to the upper part of the Hoz de Callo Conglomerates Formation of the classic Molina de Aragón area. It is interpreted as braided river deposits with paleocurrents parallel to the basin axis. The identification in this new area represents the expand of the sedimentation realm of this cycle to the SE of the Iberian Ranges.
PB Sociedad Geológica de España.
SN 1576-5172
YR 2005
FD 2005
LK https://hdl.handle.net/20.500.14352/52503
UL https://hdl.handle.net/20.500.14352/52503
LA spa
DS Docta Complutense
RD 12 abr 2025