Alloriite, Na5K1.5Ca(Si6Al6O24)(SO4)(OH)0.5
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- 作者：N. V. Chukanov (1)
R. K. Rastsvetaeva (2)
I. V. Pekov (3)
A. E. Zadov (4) - 刊名：Geology of Ore Deposits
- 出版年：2007
- 出版时间：December 2007
- 年：2007
- 卷：49
- 期：8
- 页码：752-757
- 全文大小：249KB
- 参考文献：1. P. Ballirano, A. Maras, and P. R. Buseck, “Crystal Chemistry and IR Spectroscopy of Cl-and SO4-Bearing Cancrinite-Like Minerals,-Am. Mineral. 81, 1003-012 (1996).
2. P. Ballirano, A. Maras, P. R. Buseck, et al., “Improved Powder X-Ray Data for Cancrinites: I. Afghanite,-Powder Diffraction 9(1), 68-3 (1994).
3. P. Ballirano, E. Bonaccorsi, A. Maras, and S. Merlino, “Crystal Structure of Afghanite, the Eightlayer Member of the Cancrinite Group: Evidence for Long-Range Si, Al Ordering,-Eur. J. Mineral. 9, 21-0 (1997).
4. P. Bariand, F. Cesbron, and R. Giraud, “Une Nouvelle Espéce Minerale: l’Afghanite de Sar-e-Sang, Badakhshan, Afghanistan. Comparison Avec les Minéraux du Groupe de la Cancrinite,-Bull. Soc. Franc. Miner. Gristallogr 91, 34-2 (1968).
5. E. Bonaccorsi and S. Merlino, “Modular Microporous Minerals: Cancrinite-Davyne Group and C-S-H Phases,-Reviews in Mineral. and Geochem. 57, 241-90 (2005). CrossRef
6. G. Della Ventura, F. Bellatreccia, and E. Bonaccorsi, “CO2 in Minerals of the Cancrinite-Sodalite Group: Piglianoite,-Eur. J. Mineral. 17, 847-51 (2005). CrossRef
7. E. A. Pobedimskaya, R. K. Rastsvetaeva, L. E. Terent’eva, and A. N. Sapozhnikov, “Crystal Structure of Afghanite,-Dokl. Akad. Nauk SSSR 320(4), 882-86 (1991).
8. R. K. Rastsvetaeva, E. A. Pobedimskaya, L. E. Terent’eva, and A. N. Sapozhnikov, “Structural Features of Afghanite and Its Place Among Minerals of Cancrinite Group,-Kristallografiya 38(2), 94-03 (1993). - 作者单位：N. V. Chukanov (1)
R. K. Rastsvetaeva (2)
I. V. Pekov (3)
A. E. Zadov (4)
1. Institute of Problems of Chemical Physics, Russian Academy of Sciences, Chernogolovka, Moscow oblast, 142432, Russia
2. Institute of Crystallography, Russian Academy of Sciences, Leninskii pr. 59, Moscow, 117333, Russia
3. Faculty of Geology, Moscow State University, Vorob’evy gory, 119899, Russia
4. NPO Regenerator, 3d proezd Mar’inoi Roshchi, 40, Moscow, 127018, Russia - ISSN：1555-6476
文摘
Alloriite, a new mineral species, has been found in volcanic ejecta at Mt. Cavalluccio (Campagnano municipality, Roma province, Latium region, Italy) together with sanidine, biotite, andradite, and apatite. The mineral is named in honor of Roberto Allori (b. 1933), an amateur mineralogist and prominent mineral collector who carried out extensive and detailed field mineralogical investigations of volcanoes in the Latium region. Alloriite occurs as short prismatic and tabular crystals up to 1.5 × 2 mm in size. The mineral is colorless, transparent, with a white streak and vitreous luster. Alloriite is not fluorescent and brittle; the Mohs-hardness is 5. The cleavage is imperfect parallel to {10 $\overline 1 $ 0}. The density measured with equilibration in heavy liquids is 2.35g/cm3 and calculated density (D calc) is 2.358 g/cm3 (on the basis of X-ray single-crystal data) and 2.333 g/cm3 (from X-ray powder data). Alloriite is optically uniaxial, positive, ω = 1.497(2), and ? = 1.499(2). The infrared spectrum is given. The chemical composition (electron microprobe, H2O determined using the Penfield method, CO2, with selective sorption, wt %) is: 13.55 Na2O, 6.67 K2O, 6.23 CaO, 26.45 Al2O3, 34.64 SiO2, 8.92 SO3, 0.37 Cl, 2.1 H2O, 0.7 CO2, 0.08-O = Cl2, where the total is 99.55. The empirical formula (Z = 1) is Na19.16K6.21Ca4.87(Si25.26Al22.74O96)(SO4)4.88(CO3)0.70Cl0.46(OH)0.76 · 4.73H2O. The simplified formula (taking into account the structural data, Z = 4) is: [Na(H2O)][Na4K1.5(SO4)] · [Ca(OH,Cl)0.5](Si6Al6O24). The crystal structure has been studied (R = 0.052). Alloriite is trigonal, the space group is P31c; the unit-cell dimensions are a = 12.892(3), c = 21.340(5) ?, and V = 3071.6(15) ?3. The crystal structure of alloriite is based on the same tetrahedral framework as that of afghanite. In contrast to afghanite containing clusters [Ca-Cl]+ and chains ...Ca-Cl-Ca-Cl..., the new mineral contains clusters [Na-H2O]+ and chains ...Na-H2O-Na-H2O.... The strongest reflections in the X-ray powder diffraction pattern [d, ? (I, %)(hkl)] are: 11.3(70)(100), 4.85(90)(104), 3.76(80)(300), 3.68(70)(301), 3.33(100)(214), and 2.694(70)(314, 008). The type material of alloriite is deposited in the Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow. The registration number is 3459/1.