A number of metallic (Fe, Cu, Mn, Sb) and non-metallic deposits (Mg silicates, magnesite, sericitized aplites, granite, pegmatites) have been the target of exploration and exploitation in Elba Island since the The iron deposits of Elba Island have been the target of intense exploitation since the I SI Millennium BC up to present 198 I. Elba is especially famous worldwide for its iron deposits and the pegmatitic minerals from Monte Capanne. Ali iron mines are now closed, but in the last years several steps were taken in order to preserve and promote such a valuable heritage: the inclusion of Elban mining and mineralogica! areas into the UNESCO's World Heritage provisional li st of geological sites (1990), the project of the "Elba Island Mineralogical and Mining Park" (started in 1991 and now underway), and the establishment in 1996 of the "Tuscan Archipelago National Park". In this paper we summarize the state of the art of the research on Elba Island 's minerai iron ore deposits, with particular focus onto the iron ores of eastem Elba. In the course of almost three thousand years of exploitation, not less than 60 million tons of Fe ore have been won. Fe. Notwithstanding the many studies on these deposits carried out by Italian and foreign scholars over more than two hundred years, many aspects of their setting, genes is and evolution stili need to be clarified and better constrained. This is due to various factors, including the complex (and onJy partially understood) geological framework of the island, and the closure of rnining activity, with consequent inaccessibility to many mine-workings. We stressand emphasize the some mostproblematic aspects, which are fundamental clues not only for the understanding ofof the oreforming genetic processes of and evolution of Elban 's mineraI deposits, but al so for the reconstruction of the overall geologie evolution of the Apenninic chain

The iron mineral deposits of Elba Island: state of the art / Tanelli G.; Benvenuti M.; Costagliola P.; Dini A.; Maineri C.; Mascaro I.; Lattanzi P.; Ruggieri G.. - In: OFIOLITI. - ISSN 0391-2612. - STAMPA. - 26:(2001), pp. 239-248.

The iron mineral deposits of Elba Island: state of the art

TANELLI, GIUSEPPE;BENVENUTI, MARCO;COSTAGLIOLA, PILARIO;
2001

Abstract

A number of metallic (Fe, Cu, Mn, Sb) and non-metallic deposits (Mg silicates, magnesite, sericitized aplites, granite, pegmatites) have been the target of exploration and exploitation in Elba Island since the The iron deposits of Elba Island have been the target of intense exploitation since the I SI Millennium BC up to present 198 I. Elba is especially famous worldwide for its iron deposits and the pegmatitic minerals from Monte Capanne. Ali iron mines are now closed, but in the last years several steps were taken in order to preserve and promote such a valuable heritage: the inclusion of Elban mining and mineralogica! areas into the UNESCO's World Heritage provisional li st of geological sites (1990), the project of the "Elba Island Mineralogical and Mining Park" (started in 1991 and now underway), and the establishment in 1996 of the "Tuscan Archipelago National Park". In this paper we summarize the state of the art of the research on Elba Island 's minerai iron ore deposits, with particular focus onto the iron ores of eastem Elba. In the course of almost three thousand years of exploitation, not less than 60 million tons of Fe ore have been won. Fe. Notwithstanding the many studies on these deposits carried out by Italian and foreign scholars over more than two hundred years, many aspects of their setting, genes is and evolution stili need to be clarified and better constrained. This is due to various factors, including the complex (and onJy partially understood) geological framework of the island, and the closure of rnining activity, with consequent inaccessibility to many mine-workings. We stressand emphasize the some mostproblematic aspects, which are fundamental clues not only for the understanding ofof the oreforming genetic processes of and evolution of Elban 's mineraI deposits, but al so for the reconstruction of the overall geologie evolution of the Apenninic chain
2001
26
239
248
Tanelli G.; Benvenuti M.; Costagliola P.; Dini A.; Maineri C.; Mascaro I.; Lattanzi P.; Ruggieri G.
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Utilizza questo identificatore per citare o creare un link a questa risorsa: https://hdl.handle.net/2158/313118
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