| Reference Type | Journal (article/letter/editorial) |
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| Title | Tungusite: new data, relationship with gyrolite and structural model |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Ferraris, Giovanni | Author |
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| Pavese, Alessandro | Author |
| Soboleva, Svetlana V. | Author |
| Year | 1995 (September) | Volume | 59 |
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| Issue | 396 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_59/59-396-535.pdf+ |
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| DOI | doi:10.1180/minmag.1995.059.396.13Search in ResearchGate |
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| Generate Citation Formats |
| Mindat Ref. ID | 2671 | Long-form Identifier | mindat:1:5:2671:4 |
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| GUID | 0 |
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| Full Reference | Ferraris, Giovanni, Pavese, Alessandro, Soboleva, Svetlana V. (1995) Tungusite: new data, relationship with gyrolite and structural model. Mineralogical Magazine, 59 (396) 535-543 doi:10.1180/minmag.1995.059.396.13 |
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| Plain Text | Ferraris, Giovanni, Pavese, Alessandro, Soboleva, Svetlana V. (1995) Tungusite: new data, relationship with gyrolite and structural model. Mineralogical Magazine, 59 (396) 535-543 doi:10.1180/minmag.1995.059.396.13 |
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| In | (1995, September) Mineralogical Magazine Vol. 59 (396) Mineralogical Society |
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| Abstract/Notes | AbstractNew chemical analyses, electron and X-ray powder diffraction data, and comparison with gyrolite and reyerite show that tungusite has the ideal formula , symmetry P and a = 9.714(9), b = 9.721(9), c = 22.09(3), α = 90.13(1)°, β = 98.3(2)°, γ = 120.0(1)°, Z = 1. A structural model for tungusite is derived by splitting the double tetrahedral layer of reyerite and inserting a trioctahedral X sheet which is ideally occupied by Fe2+. Polytypism phenomena due to different relative positions between tetrahedral and X sheets are discussed. A substitutional solid solution represented by the formula [Ca14(OH)8]Si24−yAlyO60[NaxM9−(x+z)□z(OH)14−(x+y+2z)·(x+y+2z)H2O] includes tungusite (x = y = z = 0, M = Fe2+ and gyrolite (x = 1, y = 1, z = 6, M = Ca). |
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