Tazzoliite, ideally Ba 2CaSr 0.5Na 0.5Ti 2Nb 3SiO 17[PO 2(OH) 2] 0.5, is a new mineral (IMA 2011-018) from Monte delle Basse, Euganei Hills, Galzignano Terme, Padova, Italy. It occurs as lamellar pale orange crystals, which are typically a few m m thick and up to 0.4 mm long, closely associated with a diopsidic pyroxene and titanite. Tazzoliite is transparent. It has a white streak, a pearly lustre, is not fluorescent and has a hardness of 6 (Mohs' scale). The tenacity is brittle and the crystals have a perfect cleavage along 010. The calculated density is 4.517 g cm -3. Tazzoliite is biaxial (-) with 2V meas of ∼50°, it is not pleochroic and the average refractive index is 2.04. No twinning was observed. Electronmicroprobe analyses gave the following chemical formula: (Ba 1.93Ca 1.20Sr 0.52Na 0.25Fe 2+0.10) Σ4(Nb 2.88Ti 2.05Ta 0.07Zr 0.01V 5+0.01) Σ5.02SiO 17[(P 0.13Si 0.12S 0.07) Σ0.32O 0.66(OH) 0.66] [F 0.09(OH) 0.23] Σ0.32. Tazzoliite is orthorhombic, space group Fmmm, with unit-cell parameters a = 7.4116(3), b = 20.0632(8), c = 21.4402(8) Å, V = 3188.2(2) Å 3 and Z = 8. The crystal structure, obtained from single-crystal X-ray diffraction data, was refined to R 1(F2) = 0.063. It consists of a framework of Nb(Ti) octahedra and BaO 7 polyhedra sharing apexes or edges, and Si tetrahedra sharing apexes with Nb(Ti) octahedra and BaO 7 polyhedra. The structure, which is related to the pyrochlore structure, contains three Nb(Ti) octahedra: two are Nb dominant and one is Ti dominant. Chains of A2O 8 polyhedra [A2 being occupied by Sr(Ca, Fe)] extend along [100] and are surrounded by Nb octahedra. Channels formed by six Nb(Ti) octahedra and two tetrahedra, or four A1O 8(OH) polyhedra (A1 being occupied by Ba), alternate along [100]. The channels are partially occupied by [PO 2(OH) 2] in two possible mutually exclusive positions, alternating with fully occupied A3O 7 polyhedral pairs [A3 being occupied by Ca(Na)]. The seven strongest X-ray powder diffraction lines [d in Å (I/I 0) (hkl)] are: 3.66 (60) (044), 3.16 (30) (153), 3.05 (100) (204), 2.98 (25) (240), 2.84 (50) (064), 1.85 (25) (400) and 1.82 (25) (268). Raman spectra of tazzoliite were collected in the range 150-3700 cm -1 and confirm the presence of OH groups. Tazzoliite is named in honour of Vittorio Tazzoli in recognition of his contributions to the fields of mineralogy and crystallography.

Tazzoliite : a new mineral with a pyrochlore-related structure from the Euganei Hills, Padova, Italy / F. Cámara, F. Nestola, L. Bindi, A. Guastoni, F. Zorzi, L. Peruzzo, D. Pedron. - In: MINERALOGICAL MAGAZINE. - ISSN 0026-461X. - 76:4(2012 Aug), pp. 827-838.

Tazzoliite : a new mineral with a pyrochlore-related structure from the Euganei Hills, Padova, Italy

F. Cámara
;
2012

Abstract

Tazzoliite, ideally Ba 2CaSr 0.5Na 0.5Ti 2Nb 3SiO 17[PO 2(OH) 2] 0.5, is a new mineral (IMA 2011-018) from Monte delle Basse, Euganei Hills, Galzignano Terme, Padova, Italy. It occurs as lamellar pale orange crystals, which are typically a few m m thick and up to 0.4 mm long, closely associated with a diopsidic pyroxene and titanite. Tazzoliite is transparent. It has a white streak, a pearly lustre, is not fluorescent and has a hardness of 6 (Mohs' scale). The tenacity is brittle and the crystals have a perfect cleavage along 010. The calculated density is 4.517 g cm -3. Tazzoliite is biaxial (-) with 2V meas of ∼50°, it is not pleochroic and the average refractive index is 2.04. No twinning was observed. Electronmicroprobe analyses gave the following chemical formula: (Ba 1.93Ca 1.20Sr 0.52Na 0.25Fe 2+0.10) Σ4(Nb 2.88Ti 2.05Ta 0.07Zr 0.01V 5+0.01) Σ5.02SiO 17[(P 0.13Si 0.12S 0.07) Σ0.32O 0.66(OH) 0.66] [F 0.09(OH) 0.23] Σ0.32. Tazzoliite is orthorhombic, space group Fmmm, with unit-cell parameters a = 7.4116(3), b = 20.0632(8), c = 21.4402(8) Å, V = 3188.2(2) Å 3 and Z = 8. The crystal structure, obtained from single-crystal X-ray diffraction data, was refined to R 1(F2) = 0.063. It consists of a framework of Nb(Ti) octahedra and BaO 7 polyhedra sharing apexes or edges, and Si tetrahedra sharing apexes with Nb(Ti) octahedra and BaO 7 polyhedra. The structure, which is related to the pyrochlore structure, contains three Nb(Ti) octahedra: two are Nb dominant and one is Ti dominant. Chains of A2O 8 polyhedra [A2 being occupied by Sr(Ca, Fe)] extend along [100] and are surrounded by Nb octahedra. Channels formed by six Nb(Ti) octahedra and two tetrahedra, or four A1O 8(OH) polyhedra (A1 being occupied by Ba), alternate along [100]. The channels are partially occupied by [PO 2(OH) 2] in two possible mutually exclusive positions, alternating with fully occupied A3O 7 polyhedral pairs [A3 being occupied by Ca(Na)]. The seven strongest X-ray powder diffraction lines [d in Å (I/I 0) (hkl)] are: 3.66 (60) (044), 3.16 (30) (153), 3.05 (100) (204), 2.98 (25) (240), 2.84 (50) (064), 1.85 (25) (400) and 1.82 (25) (268). Raman spectra of tazzoliite were collected in the range 150-3700 cm -1 and confirm the presence of OH groups. Tazzoliite is named in honour of Vittorio Tazzoli in recognition of his contributions to the fields of mineralogy and crystallography.
No
English
crystal structure; Euganei Hills; new mineral; pyrochlore; Raman spectroscopy; Tazzoliite
Settore GEO/06 - Mineralogia
Articolo
Esperti anonimi
Ricerca di base
Pubblicazione scientifica
ago-2012
Mineralogical Society of Great Britain
76
4
827
838
12
Pubblicato
Periodico con rilevanza internazionale
Aderisco
info:eu-repo/semantics/article
Tazzoliite : a new mineral with a pyrochlore-related structure from the Euganei Hills, Padova, Italy / F. Cámara, F. Nestola, L. Bindi, A. Guastoni, F. Zorzi, L. Peruzzo, D. Pedron. - In: MINERALOGICAL MAGAZINE. - ISSN 0026-461X. - 76:4(2012 Aug), pp. 827-838.
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Prodotti della ricerca::01 - Articolo su periodico
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262
Article (author)
si
F. Cámara, F. Nestola, L. Bindi, A. Guastoni, F. Zorzi, L. Peruzzo, D. Pedron
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/474913
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