Rüdlingerite, Mn2+2V5+As5+O7·2H2O, a New Species Isostructural with Fianelite

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)

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

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::be50bba29079529638b847428b731c9d

Te-rich canfieldite, AG8SN(S,TE)6, from the Legenbach Quarry, Binntal, Canton Valais, Switzerland: Occurrence, description and crystal structure

Autor: Bindi L. [1, 2], Nestola F.[3], Guastoni A. [4], Zorzi F. [3], Peruzzo L. [5], Raber T.

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

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/

Fassinaite, Pb22+(S6+O3S2-)(C4+O3), the first mineral with coexisting carbonate and thiosulfate groups: Description and crystal structure

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

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

Crystallographic Methods for Non-destructive Characterization of Mineral Inclusions in Diamonds

Autor: Ross J. Angel, Matteo Alvaro, Fabrizio Nestola

Publikováno v: Reviews in mineralogy and geochemistry 88 (2022): 257–306. doi:10.2138/rmg.2022.88.05
info:cnr-pdr/source/autori:Angel R.J.[1], Alvaro M.[2], Nestola F.[3]/titolo:Crystallographic Methods for Non-destructive Characterization of Mineral Inclusions in Diamonds/doi:10.2138%2Frmg.2022.88.05/rivista:Reviews in mineralogy and geochemistry/anno:2022/pagina_da:257/pagina_a:306/intervallo_pagine:257–306/volume:88

The mineralogy and chemical compositions of inclusions in diamonds are the primary source of information about the environment in which diamonds grow and help constrain the mechanisms of their growth. However, the vast majority of the information abo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4e0aa83ddd028830a6c4d041403c5ff4

The role of Fe content on the Fe-Mg exchange reaction in augite

Autor: Fabrizio Nestola, Chiara Domeneghetti, Matteo Alvaro, Mara Murri, Lorenzo Scandolo, A. M. Fioretti

Publikováno v: The American mineralogist (Online) 101 (2016): 2747–2750.
info:cnr-pdr/source/autori:Murri M.[1], Scandolo L.[1], Fioretti A.[2], Nestola F.[3], Domeneghetti C.[1], Alvaro M.[1]/titolo:The role of Fe content on the Fe-Mg exchange reaction in augite./doi:/rivista:The American mineralogist (Online)/anno:2016/pagina_da:2747/pagina_a:2750/intervallo_pagine:2747–2750/volume:101

The study of the intracrystalline Fe-Mg exchange between M 1 and M 2 crystallographic sites in clinopyroxene on samples a variety of geological settings has provided a framework to understand the thermal history of pyroxene-bearing rocks. The Fe-Mg e

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ff7be9145c85219e2e034985d38b8370
http://hdl.handle.net/11577/3219870