García Veigas, JavierOrtí, FedericoRosell, L.Inglés, M.2017-07-262017-07-261994http://hdl.handle.net/10272/13981The mineralogical, petrological and geochemical characteristics of this saline unit indicate that the halite sedimentation took place in a subsiding shallow marine basin where contributions of continental and minor hydrothermal waters were available. Starting from the bromine distribution and fluid inclusions composition in the halite samples a correlation of both boreholes is proposedspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/EvaporiteHaliteFluid inclusionMessinianLorca basinCaracterización petrológica y geoquímica de la Unidad Salina messimense de la cuenca de Lorca (sondeos S4 y S5)Petrological and geochemical characterization of the Messinian Saline Unit in Lorca basin (boreholes S4 and S5)journal articleopen access