RT Journal Article
T1 Datación magnetoestratigráfica de las evaporitas de la cuenca neógena de Fortuna (Murcia)
T1 Magneloslratigraphy of llie evaporites from the Neogene Fortuna Basin (Murcia)
A1 Playà, Elisabet
A1 Dinarès Turell, Jaume
A1 Ortí, Federico
A1 Gomis Coll, E.
A1 Rosell, L.
AB The magnetostratigraphic study of the Río Chicamo section (240 m) in the Neogene Fortuna Basin (Murcia,Eastern Betics) has enabled the record of five magnetozones. The possible correlations with the standard geomagnetic polarity time scale (CPTS) imply that the evaporitic succession of the Fortuna Basin was not coeval with the Messinian evaporites of the Sorbas (Almeria, Spain) and Caltanissetta (central Sicily) basins, which were assigned to the reverse chron C3r (Gautier et alv 1994). The marine evaporites of the Fortuna Basin are older (Tortonian-Messinian boundary or early Messinian) than the evaporites of those basins and, therefore, cannot be assigned to the main upper Messinian evaporite event of the Mediterranean region
PB Sociedad Geológica de España
YR 1998
FD 1998
LK http://hdl.handle.net/10272/10162
UL http://hdl.handle.net/10272/10162
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 15 jun 2026