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pro vyhledávání: '"Maineri C. (2"'
Autor:
Lattanzi P. (1), Benvenuti M. (2), Costagliola P. (2), Maineri C. (2), Mascaro I. (2), Tanelli G. (2), Dini A. (3), Ruggieri G. (4)
Publikováno v:
Tenth International Symposium on Water-Rock Interaction, pp. 725–728, Villasimius, Italy, 10-15 July 2001
info:cnr-pdr/source/autori:Lattanzi P. (1), Benvenuti M. (2), Costagliola P. (2), Maineri C. (2), Mascaro I. (2), Tanelli G. (2), Dini A. (3), Ruggieri G. (4)/congresso_nome:Tenth International Symposium on Water-Rock Interaction/congresso_luogo:Villasimius, Italy/congresso_data:10-15 July 2001/anno:2001/pagina_da:725/pagina_a:728/intervallo_pagine:725–728
info:cnr-pdr/source/autori:Lattanzi P. (1), Benvenuti M. (2), Costagliola P. (2), Maineri C. (2), Mascaro I. (2), Tanelli G. (2), Dini A. (3), Ruggieri G. (4)/congresso_nome:Tenth International Symposium on Water-Rock Interaction/congresso_luogo:Villasimius, Italy/congresso_data:10-15 July 2001/anno:2001/pagina_da:725/pagina_a:728/intervallo_pagine:725–728
Ceramic raw material in Tuscany is currently mined in four main deposits (Marciana and La Crocetta in Elba Island, Botro ai Marmi near Campiglia Marittima, and Piloni di Torniella near Roccastrada). The deposits are associated with magmatic rocks of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::1ae1f036673f2c22a3315d9c50678a64
https://publications.cnr.it/doc/214076
https://publications.cnr.it/doc/214076
Publikováno v:
Mineralogical magazine
63 (1999): 111–122. doi:10.1180/minmag.1999.063.1.11
info:cnr-pdr/source/autori:Costagliola P. (1), Benvenuti M. (2,3), Maineri C. (2,3), Lattanzi P. (3,4), Ruggieri G. (5)/titolo:Fluid circulation in the Apuane Alps core complex; evidence from extension veins in the Carrara Marble/doi:10.1180%2Fminmag.1999.063.1.11/rivista:Mineralogical magazine (Print)/anno:1999/pagina_da:111/pagina_a:122/intervallo_pagine:111–122/volume:63
63 (1999): 111–122. doi:10.1180/minmag.1999.063.1.11
info:cnr-pdr/source/autori:Costagliola P. (1), Benvenuti M. (2,3), Maineri C. (2,3), Lattanzi P. (3,4), Ruggieri G. (5)/titolo:Fluid circulation in the Apuane Alps core complex; evidence from extension veins in the Carrara Marble/doi:10.1180%2Fminmag.1999.063.1.11/rivista:Mineralogical magazine (Print)/anno:1999/pagina_da:111/pagina_a:122/intervallo_pagine:111–122/volume:63
In the Apuane Alps (AA) metamorphic core complex, syn-metamorphic mineral deposits are mainly restricted to extensional shear zones in the Lower Plate Palaeozoic basement. By contrast, the extension structures at upper levels, such as the detachment
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3174b46c09eae9038202e40c1d5d4fe0