| Reference Type | Journal (article/letter/editorial) |
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| Title | Cesanite, Ca2Na3[(OH)(SO4)3], a sulphate isotypic to apatite, from the Cesano geothermal field (Latium, Italy) |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Cavarretta, G. | Author |
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| Mottana, A. | Author |
| Tecce, F. | Author |
| Year | 1981 (September) | Volume | 44 |
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| Page(s) | 269-273 | Issue | 335 |
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| Publisher | Mineralogical Society |
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| URL | |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_44/44-335-269.pdf+ |
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| DOI | doi:10.1180/minmag.1981.044.335.05Search in ResearchGate |
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| Generate Citation Formats |
| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 3270 | Long-form Identifier | mindat:1:5:3270:8 |
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| GUID | 0 |
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| Full Reference | Cavarretta, G.; Mottana, A.; Tecce, F. (1981) Cesanite, Ca2Na3[(OH)(SO4)3], a sulphate isotypic to apatite, from the Cesano geothermal field (Latium, Italy). Mineralogical Magazine, 44 (335). 269-273 doi:10.1180/minmag.1981.044.335.05 |
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| Plain Text | Cavarretta, G.; Mottana, A.; Tecce, F. (1981) Cesanite, Ca2Na3[(OH)(SO4)3], a sulphate isotypic to apatite, from the Cesano geothermal field (Latium, Italy). Mineralogical Magazine, 44 (335). 269-273 doi:10.1180/minmag.1981.044.335.05 |
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| In | (1981, September) Mineralogical Magazine Vol. 44 (335) Mineralogical Society |
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| Abstract/Notes | AbstractCesanite occurs both as a solid vein (1 cm thick) and as a cavity-filling of an explosive breccia in core samples of the Cesano 1 geothermal well (Cesano area, Latium, Italy).Cesanite is coloudess, medium to coarse grained, soft (H = 2 to 3) and light (ρmeas 2.786±0.002 g cm−3). It is uniaxial negative, ε = 1.564, ω = 1.570, with space group P63/m and cell parameters a = 9.442 (4), c = 6.903 (3) Å, for c/a = 0.730. Identifying spacings are 8.161, 2.822, 2.727,1.844 Å, in X-ray powder patterns strikingly similar to those of apatite. The chemical formula (microprobe analyses on two grains) is Ca1.53Sr0.03Na3.42K0.02[(Cl0.06F0.06OH0.44)(S2.99O12)]·0.44H2O, while the theoretical formula, derived from considerations on structural identity with apatite, is Ca2Na3[(OH)(SO4)3]. Cesanite is the end member of the apatite-wilkeite ellestadite series where [PO4]3− is entirely substituted by [SO4]2−, the charge balance being made up by Na+ substituting for Ca2+. |
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