Resumen de Caracterización petrológica y geoquímica de la Unidad Salina messiniense de la cuenca de Lorca (sondeos S4 y S5).

Javier García Veigas, Federico Ortí Cabo, Laura Rosell Ortiz, Montserrat Inglès Urpinell

• The 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 proposed