Resumen de Aspectos geológicos y metalogenéticos del área de Herrera de los Navarros (Cadena Ibérica Oriental, Zaragoza-Teruel)
Esteve Cardellach i López, Josefina Besteiro Rafales, María Cinta Osácar Soriano, Andrés Pocoví Juan
In the Herrera de los Navarros area several mineral occurrences ranging from vein type (Ba,Pb-Zn,Sb) to stratabound (Zn (Pb)) are found. They are placed within Paleozoic materials and appear to be structurally controled by a thrust phase related to Hercynian orogeny which developped a fracture system after the first phase folds. Thus, mineralized veins are found arround periclinal edges of folds. A litological control from devonian limestones and ashgillian dolomites has also been observed.
