@article{10272/13464,
year = {1995},
url = {http://hdl.handle.net/10272/13464},
abstract = {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},
publisher = {Sociedad Geológica de España},
title = {Composición isotópica de los yesos Messinienses de la cuenca de Fortuna (Murcia): implicaciones sedimentológicas},
title = {Isotopic composition of Messinian gypsum in the Fortuna basin (Murcia): sedimentological significance},
author = {Playà, Elisabet and Ortí, Federico and Rosell, L.},
}