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Akademický článek
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Autor:
Cámara F.[1], Ciriotti M.E.[2, Kolitsch U.[4, Bosi F.[6, Bittarello E.[3, Brizio P.[9], Vignola P.[10], Blass G.[11]
Publikováno v:
Mineralogical magazine
85 (2021): 901–909. doi:10.1180/mgm.2021.84
info:cnr-pdr/source/autori:Cámara F.[1], Ciriotti M.E.[2,3], Kolitsch U.[4,5], Bosi F.[6,7], Bittarello E.[3,8], Brizio P.[9], Vignola P.[10], Blass G.[11]/titolo:Armellinoite-(Ce), Ca4Ce4+(AsO4)4 .H2O, a new mineral species isostructural with pottsite, (Pb3Bi)Bi(VO4)4 .H2O/doi:10.1180%2Fmgm.2021.84/rivista:Mineralogical magazine (Print)/anno:2021/pagina_da:901/pagina_a:909/intervallo_pagine:901–909/volume:85
85 (2021): 901–909. doi:10.1180/mgm.2021.84
info:cnr-pdr/source/autori:Cámara F.[1], Ciriotti M.E.[2,3], Kolitsch U.[4,5], Bosi F.[6,7], Bittarello E.[3,8], Brizio P.[9], Vignola P.[10], Blass G.[11]/titolo:Armellinoite-(Ce), Ca4Ce4+(AsO4)4 .H2O, a new mineral species isostructural with pottsite, (Pb3Bi)Bi(VO4)4 .H2O/doi:10.1180%2Fmgm.2021.84/rivista:Mineralogical magazine (Print)/anno:2021/pagina_da:901/pagina_a:909/intervallo_pagine:901–909/volume:85
Armellinoite-(Ce), ideally Ca4Ce4+(AsO4)4⋅H2O, is a new mineral discovered in Fe–Mn ore in metaquartzites of the Montaldo mine, Corsaglia Valley, Cuneo Province, Piedmont, Italy. It occurs as very small and rare, pale yellow to brown–yellow pse
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0bad97e58e2992f34893e97ba350df2e
http://hdl.handle.net/11573/1616712
http://hdl.handle.net/11573/1616712
The Lavrion area corresponds to the western part of the Attic-Cycladic metamorphic belt, in the back-arc region of the active Hellenic subduction zone. Between the Eocene and the Miocene, metamorphic rocks (mainly marbles and schists) underwent sever
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::5116bff4c6dd86af48a609ee6adf4716
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3068567
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3068567
Autor:
Fleck M., Kolitsch U.
Publikováno v:
Zeitschrift für Kristallographie - New Crystal Structures, Vol 217, Iss 1, Pp 471-473 (2002)
Externí odkaz:
https://doaj.org/article/ac3f7a165e2d413389791716348d6f55
Publikováno v:
Mineralogical magazine
82 (2018): 1374. doi:10.1180/mgm.2018.161
info:cnr-pdr/source/autori:Cámara F., Ciriotti M.E., Kolitsch U., Bosi F, Bittarello E, Brizio P, Vignola P, Blass G./titolo:Armellinoite-(Ce), IMA 2018-094/doi:10.1180%2Fmgm.2018.161/rivista:Mineralogical magazine (Print)/anno:2018/pagina_da:1374/pagina_a:/intervallo_pagine:1374/volume:82
82 (2018): 1374. doi:10.1180/mgm.2018.161
info:cnr-pdr/source/autori:Cámara F., Ciriotti M.E., Kolitsch U., Bosi F, Bittarello E, Brizio P, Vignola P, Blass G./titolo:Armellinoite-(Ce), IMA 2018-094/doi:10.1180%2Fmgm.2018.161/rivista:Mineralogical magazine (Print)/anno:2018/pagina_da:1374/pagina_a:/intervallo_pagine:1374/volume:82
Armellinoite-(Ce) Ca4Ce4+(AsO4)4·H2O In the dumps of the Montaldo di Mondovì mine, Frazze Rocconi, Borgata Oberti, Montaldo di Mondovì (CN), Corsaglia Valley, Piedmont, Italy (44°19?28?N, 7°51?8?E). Isostructural with pottsite Tetragonal: I41/a;
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::ae5c720f5c98ae9dde7fbe913294f6f4
http://www.cnr.it/prodotto/i/400517
http://www.cnr.it/prodotto/i/400517
Akademický článek
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Publikováno v:
In Journal of Alloys and Compounds 6 October 2004 379(1-2):103-109
Autor:
Kolitsch U.
Publikováno v:
Zeitschrift für Kristallographie - New Crystal Structures, Vol 219, Iss 1-4, Pp 227-228 (2004)
Externí odkaz:
https://doaj.org/article/2b08bea444554ecdad0c3bad7b075820
Autor:
Kolitsch U.
Publikováno v:
Zeitschrift für Kristallographie - New Crystal Structures, Vol 218, Iss 4, Pp 401-402 (2003)
Cr2O7Rb2, triclinic, P1̅ (No. 2), a = 7.433(1) Å, b = 7.571(2) Å, c = 7.832(2) Å, α = 109.44(3)°, β = 90.81(3)°, γ = 108.89(3)°, V = 389.6 Å3, Z = 2, Rgt(F) = 0.028, wRref(F2) = 0.076, T = 293 K.
Externí odkaz:
https://doaj.org/article/b7cb15bd9cb94d018afd5c7906fd27de
Vein-type Pb-Ni-Bi-Au-Ag mineralization at the Clemence deposit in the Kamariza and “km3” in the Lavrion area, was synchronous with the intrusion of a Miocene granodiorite body and related felsic and mafic dikes and sills within marbles and schis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::5f1f396f20399a7447b1322f985d651d
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069126
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069126