RT Journal Article
T1 El Cretácico terminal y Paleoceno de la Sierra del Carche (dominio prebético, Jumilla). Caracterización estratigráfica y sedimentológica
T2 Latest Cretaceous and Paleocene rocks of Sierra del Carche (Prebetic domain, Jumilla). Stratigraphic and sedimentological analyses
A1 Chacón Pichaco, Beatriz
A1 Martín Chivelet, Javier
AB The mid Campanian to Paleocene section in Sierra del Carche (Jumilla, Prebetic Domain, SE Spain) consists of 125 meters of carbonates and marls deposited in open platform environments. Facies analysis of these rocks characterize three major unconformities (mid Maastrichtian, latest Maastrichtian to earliest Paleocene, and mid Pa/eocene in age), and define the main changes in bathyrnetry occurring throughout the basin during this time. The establishment of unconformities and water-depth trends is important because of the privileged paleogeographic location occupied by the Sierra del Carche within the Betic Margin: an intermediate position betweeni the deeper facies of the Subbetic Domain (to the southeast) and the shallower sediments of other areas of the Prebetic Domain (to the northwest). Thus, the results of this work provide a good stratigraphic basis for intrabasinal correlation.
PB Sociedad Geológica de España
SN 0213-683X
YR 1999
FD 1999
LK https://hdl.handle.net/20.500.14352/111125
UL https://hdl.handle.net/20.500.14352/111125
LA spa
NO Chacón Pichaco, B. y Martín Chivelet, J. (1999) «El Cretácico terminal y Paleoceno de la Sierra del Carche (dominio prebético, Jumilla). Caracterización estratigráfica y sedimentológica», Geogaceta, 26, pp. 11-14.
DS Docta Complutense
RD 9 abr 2025