Resumen de Morfología y asociación mineralógica del yacimiento de Sb de Lanzuela (Teruel)

Antonio López Ciriano, Ignacio Subías Pérez, Constanza Fernández Nieto

• The Sb-Pb ore deposit from Lanzuela are deposed in a shear zone and related fractures. The Sb-Pb sulfosalts have been identified by X-ray diffraction, ore microscopy and electron microprobe. The mineral succession is formed by there stages: an early stages: an early stage (Fe-Sb) characterized by pyrite, stibnite and marcasite, and intermediate stage (Sb-Pb-Zn-Ag-Ba) constituted by fülöppita, zinckenite arsenopyrite, miargirite, galena, sphalerite and barite, and a remobilization stage characterized by semseyite and bournonite.