RT Journal Article
T1 Composición isotópica de los yesos Messinienses de la cuenca de Fortuna (Murcia): implicaciones sedimentológicas
T1 Isotopic composition of Messinian gypsum in the Fortuna basin (Murcia): sedimentological significance
A1 Playà, Elisabet
A1 Ortí, Federico
A1 Rosell, L.
AB Isotopic composition ('5,sO/ <5” S) o f gypsum forming the three evaporitic units o f the Fortuna basin reveals the marine or continental origin of these deposits. In contrast to previous interpretations, a sedimentation in continental and transitional environments was frequent during the Messinian evaporitic period, always in very shallow environments. Dissolution and reprecipitation of Triassic evaporites was a common mechanism producing saline solutions in the basin
PB Sociedad Geológica de España
YR 1995
FD 1995
LK http://hdl.handle.net/10272/13464
UL http://hdl.handle.net/10272/13464
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 14 jul 2026