Aspectos geológicos y metalogenéticos del área de Herrera de los Navarros (Cadena Ibérica Oriental, Zaragoza-Teruel)

• Autores: Esteve Cardellach i López, Josefina Besteiro Rafales, María Cinta Osácar Soriano, Andrés Pocoví Juan
• Localización: Boletín de la Sociedad Española de Mineralogía, ISSN 0210-6558, Vol. 11, Nº 2, 1988, págs. 84-87
• Idioma: español
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• Resumen

  • 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.