Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Nestola F.[3]"'
Autor:
Roth P.[1], Meisser N.[2], Nestola F.[3], koda R.[4], Cámara F.[5], Bosi F.[6, Ciriotti M.E.[8, Hålenius U.[10], Schnyder C.[2, 11], Bracco R.[12]
Publikováno v:
Minerals, vol. 10, no. 11, pp. 960
Minerals
Volume 10
Issue 11
Minerals, Vol 10, Iss 960, p 960 (2020)
Minerals (Basel) 10 (2020): 1–15. doi:10.3390/min10110960
info:cnr-pdr/source/autori:Roth P.[1], Meisser N.[2], Nestola F.[3], ?koda R.[4], Cámara F.[5], Bosi F.[6,7], Ciriotti M.E.[8,9], Hålenius U.[10], Schnyder C.[2,11], Bracco R.[12]/titolo:Rüdlingerite, Mn2+ 2V5+As5+O7·2H2O, a New Species Isostructural with Fianelite/doi:10.3390%2Fmin10110960/rivista:Minerals (Basel)/anno:2020/pagina_da:1/pagina_a:15/intervallo_pagine:1–15/volume:10
Minerals, 10 (11)
Minerals
Volume 10
Issue 11
Minerals, Vol 10, Iss 960, p 960 (2020)
Minerals (Basel) 10 (2020): 1–15. doi:10.3390/min10110960
info:cnr-pdr/source/autori:Roth P.[1], Meisser N.[2], Nestola F.[3], ?koda R.[4], Cámara F.[5], Bosi F.[6,7], Ciriotti M.E.[8,9], Hålenius U.[10], Schnyder C.[2,11], Bracco R.[12]/titolo:Rüdlingerite, Mn2+ 2V5+As5+O7·2H2O, a New Species Isostructural with Fianelite/doi:10.3390%2Fmin10110960/rivista:Minerals (Basel)/anno:2020/pagina_da:1/pagina_a:15/intervallo_pagine:1–15/volume:10
Minerals, 10 (11)
The new mineral species rü
dlingerite, ideally Mn2+2V5+As5+O7·
2H2O, occurs in the Fianel mine, in Val Ferrera, Grisons, Switzerland, a small Alpine metamorphic Mn deposit. It is associated with ansermetite and Fe oxyhydroxide in
dlingerite, ideally Mn2+2V5+As5+O7·
2H2O, occurs in the Fianel mine, in Val Ferrera, Grisons, Switzerland, a small Alpine metamorphic Mn deposit. It is associated with ansermetite and Fe oxyhydroxide in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::be50bba29079529638b847428b731c9d
Publikováno v:
European journal of mineralogy
26 (2014): 427–437. doi:10.1127/0935-1221/2014/0026-2382
info:cnr-pdr/source/autori:Biagioni C.[1], Orlandi P. [1,2], Pasero M.[1], Nestola F.[3], Bindi L. [4]/titolo:Mapiquiroite, (Sr,Pb)(U,Y)Fe2(Ti,Fe3+) 18O38, a new member of the crichtonite group from the Apuan Alps, Tuscany, Italy/doi:10.1127%2F0935-1221%2F2014%2F0026-2382/rivista:European journal of mineralogy (Print)/anno:2014/pagina_da:427/pagina_a:437/intervallo_pagine:427–437/volume:26
26 (2014): 427–437. doi:10.1127/0935-1221/2014/0026-2382
info:cnr-pdr/source/autori:Biagioni C.[1], Orlandi P. [1,2], Pasero M.[1], Nestola F.[3], Bindi L. [4]/titolo:Mapiquiroite, (Sr,Pb)(U,Y)Fe2(Ti,Fe3+) 18O38, a new member of the crichtonite group from the Apuan Alps, Tuscany, Italy/doi:10.1127%2F0935-1221%2F2014%2F0026-2382/rivista:European journal of mineralogy (Print)/anno:2014/pagina_da:427/pagina_a:437/intervallo_pagine:427–437/volume:26
Mapiquiroite, (Sr,Pb)(U,Y)Fe 2 (Ti,Fe 3+ ) 18 O 38 , was identified as a new mineral from the baryte + pyrite + iron oxide ores of Buca della Vena (BdV) and Monte Arsiccio (MA) mines, Apuan Alps, Tuscany, Italy. At BdV, mapiquiroite occurs as complex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3cf02d4a3464f4ece7513883e9c8dce3
http://hdl.handle.net/11568/491078
http://hdl.handle.net/11568/491078
Publikováno v:
Canadian mineralogist (Online) 50 (2012): 111–118.
info:cnr-pdr/source/autori:Bindi L. [1, 2]; Nestola F.[3]; Guastoni A. [4]; Zorzi F. [3]; Peruzzo L. [5], Raber T./titolo:Te-rich canfieldite, AG8SN(S,TE)6, from the Legenbach Quarry, Binntal, Canton Valais, Switzerland: Occurrence, description and crystal structure./doi:/rivista:Canadian mineralogist (Online)/anno:2012/pagina_da:111/pagina_a:118/intervallo_pagine:111–118/volume:50
info:cnr-pdr/source/autori:Bindi L. [1, 2]; Nestola F.[3]; Guastoni A. [4]; Zorzi F. [3]; Peruzzo L. [5], Raber T./titolo:Te-rich canfieldite, AG8SN(S,TE)6, from the Legenbach Quarry, Binntal, Canton Valais, Switzerland: Occurrence, description and crystal structure./doi:/rivista:Canadian mineralogist (Online)/anno:2012/pagina_da:111/pagina_a:118/intervallo_pagine:111–118/volume:50
In order to evaluate the effects of Te-for-S substitution in the minerals of the argyrodite group, the crystal structure and chemical composition of a crystal of Te-rich canfieldite from the Lengenbach quarry, Binntal, Switzerland, was investigated.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::aac3e75de783f7dd3844b7e0e80ab38b
http://www.mineralogicalassociation.ca/template/EJournal/
http://www.mineralogicalassociation.ca/template/EJournal/
Autor:
Bindi L. [1, 2], Nestola F. [3], Guastoni A. [4], Peruzzo L. [5], Ecker M.[6], Carampin R. [5]
Publikováno v:
Mineralogical magazine (Online) 76 (2012): 1153–1163.
info:cnr-pdr/source/autori:Bindi L. [1, 2]; Nestola F. [3]; Guastoni A. [4]; Peruzzo L. [5]; Ecker M.[6]; Carampin R. [5]/titolo:Raberite, Tl5Ag4As6SbS15, a new Tl-bearing sulfosalt from Lengenbach quarry, Binn valley, Switzerland: description and crystal structure./doi:/rivista:Mineralogical magazine (Online)/anno:2012/pagina_da:1153/pagina_a:1163/intervallo_pagine:1153–1163/volume:76
info:cnr-pdr/source/autori:Bindi L. [1, 2]; Nestola F. [3]; Guastoni A. [4]; Peruzzo L. [5]; Ecker M.[6]; Carampin R. [5]/titolo:Raberite, Tl5Ag4As6SbS15, a new Tl-bearing sulfosalt from Lengenbach quarry, Binn valley, Switzerland: description and crystal structure./doi:/rivista:Mineralogical magazine (Online)/anno:2012/pagina_da:1153/pagina_a:1163/intervallo_pagine:1153–1163/volume:76
Raberite, ideally Tl5Ag4As6SbS15, is a new mineral from Lengenbach quarry in the Binn Valley, Valais, Switzerland. It occurs very rarely as euhedral crystals up to 150 ?m across associated with yellow needle-like smithite, realgar, hatchite and proba
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::1639c4dea5b3e40feb39e7a507a25336
https://publications.cnr.it/doc/208366
https://publications.cnr.it/doc/208366
Autor:
Bindi, L. [ 1,2 ], Nestola, F. [ 3 ], Kolitsch, U. [ 4,5 ], Guastoni, A. [ 6 ], Zorzi, F. [ 3 ]
Publikováno v:
Mineralogical magazine
75 (2011): 2721. doi:10.1180/minmag.2011.075.6.2721
info:cnr-pdr/source/autori:Bindi, L. [ 1,2 ] ; Nestola, F. [ 3 ] ; Kolitsch, U. [ 4,5 ] ; Guastoni, A. [ 6 ] ; Zorzi, F. [ 3 ]/titolo:Fassinaite, Pb22+(S6+O3S2-)(C4+O3), the first mineral with coexisting carbonate and thiosulfate groups: Description and crystal structure./doi:10.1180%2Fminmag.2011.075.6.2721/rivista:Mineralogical magazine (Print)/anno:2011/pagina_da:2721/pagina_a:/intervallo_pagine:2721/volume:75
75 (2011): 2721. doi:10.1180/minmag.2011.075.6.2721
info:cnr-pdr/source/autori:Bindi, L. [ 1,2 ] ; Nestola, F. [ 3 ] ; Kolitsch, U. [ 4,5 ] ; Guastoni, A. [ 6 ] ; Zorzi, F. [ 3 ]/titolo:Fassinaite, Pb22+(S6+O3S2-)(C4+O3), the first mineral with coexisting carbonate and thiosulfate groups: Description and crystal structure./doi:10.1180%2Fminmag.2011.075.6.2721/rivista:Mineralogical magazine (Print)/anno:2011/pagina_da:2721/pagina_a:/intervallo_pagine:2721/volume:75
Fassinaite, ideally Pb-2(2+)(S2O3)(CO3), is a new mineral from the Trentini mine, Mount Naro, Vicenza Province, Veneto, Italy (holotype locality). It is also reported from the Erasmus adit, Schwarzleo District, Leogang, Salzburg, Austria and the Frie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::ea055ef2c5561def351a1fe28b35b98d
http://www.cnr.it/prodotto/i/201217
http://www.cnr.it/prodotto/i/201217