Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Lattanzi P. (3"'
Publikováno v:
Applied geochemistry 117 (2020): 1–9. doi:10.1016/j.apgeochem.2020.104600
info:cnr-pdr/source/autori:Pribil M.J.[1], Rimondi V.[2,3], Costagliola P.[2,3], Lattanzi P.[3], Rutherford D.L.[1]/titolo:Assessing mercury distribution using isotopic fractionation of mercury processes and sources adjacent and downstream of a legacy mine district in Tuscany, Italy/doi:10.1016%2Fj.apgeochem.2020.104600/rivista:Applied geochemistry/anno:2020/pagina_da:1/pagina_a:9/intervallo_pagine:1–9/volume:117
info:cnr-pdr/source/autori:Pribil M.J.[1], Rimondi V.[2,3], Costagliola P.[2,3], Lattanzi P.[3], Rutherford D.L.[1]/titolo:Assessing mercury distribution using isotopic fractionation of mercury processes and sources adjacent and downstream of a legacy mine district in Tuscany, Italy/doi:10.1016%2Fj.apgeochem.2020.104600/rivista:Applied geochemistry/anno:2020/pagina_da:1/pagina_a:9/intervallo_pagine:1–9/volume:117
Mercury (Hg) concentrations and isotopic compositions in a range of sample types collected from the legacy Abbadia San Salvatore Mine (ASSM) area were used to evaluate the distribution of Hg in the region. The district generated more than 100,000 met
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bab1e4e96b59c9ca561abb6507c30713
https://doi.org/10.1016/j.apgeochem.2020.104600
https://doi.org/10.1016/j.apgeochem.2020.104600
Publikováno v:
Rendiconti online Società Geologica Italiana 31 (2014): 223–223. doi:10.3301/ROL.2014.14
info:cnr-pdr/source/autori:Moroni M. (1), Ruggieri G. (2), Lattanzi P. (3), De Giudici G. (3)/titolo:Polyphase ore deposition at the Montevecchio vein system, SW Sardinia/doi:10.3301%2FROL.2014.14/rivista:Rendiconti online Società Geologica Italiana/anno:2014/pagina_da:223/pagina_a:223/intervallo_pagine:223–223/volume:31
info:cnr-pdr/source/autori:Moroni M. (1), Ruggieri G. (2), Lattanzi P. (3), De Giudici G. (3)/titolo:Polyphase ore deposition at the Montevecchio vein system, SW Sardinia/doi:10.3301%2FROL.2014.14/rivista:Rendiconti online Società Geologica Italiana/anno:2014/pagina_da:223/pagina_a:223/intervallo_pagine:223–223/volume:31
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::3e2f9afef936ec990ffd438f5c855284
Autor:
Tanelli G. (1), Benvenuti M. (1), Costagliola P. (1), Dini A. (2), Lattanzi P. (3), Maineri C. (1), Mascaro I. (1), Ruggieri G. (4)
Publikováno v:
Ofioliti (Bologna) 26 (2001): 239–248. doi:10.4454/ofioliti.v26i2a.148
info:cnr-pdr/source/autori:Tanelli G. (1), Benvenuti M. (1), Costagliola P. (1), Dini A. (2), Lattanzi P. (3), Maineri C. (1), Mascaro I. (1), Ruggieri G. (4)/titolo:The iron mineral deposits of Elba Island: state of art/doi:10.4454%2Fofioliti.v26i2a.148/rivista:Ofioliti (Bologna)/anno:2001/pagina_da:239/pagina_a:248/intervallo_pagine:239–248/volume:26
info:cnr-pdr/source/autori:Tanelli G. (1), Benvenuti M. (1), Costagliola P. (1), Dini A. (2), Lattanzi P. (3), Maineri C. (1), Mascaro I. (1), Ruggieri G. (4)/titolo:The iron mineral deposits of Elba Island: state of art/doi:10.4454%2Fofioliti.v26i2a.148/rivista:Ofioliti (Bologna)/anno:2001/pagina_da:239/pagina_a:248/intervallo_pagine:239–248/volume:26
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 be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::6e4049d02c4940acc07e7646805cbc67
http://www.cnr.it/prodotto/i/202753
http://www.cnr.it/prodotto/i/202753
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