| Reference Type | Journal (article/letter/editorial) |
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| Title | X-ray characterization of Mg, Fe, and Mn natural end-members of the axinite group |
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| Journal | Powder Diffraction |
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| Authors | Salviulo, Gabriella | Author |
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| Andreozzi, Giovanni B. | Author |
| Graziani, Giorgio | Author |
| Year | 2000 (September) | Volume | 15 |
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| Page(s) | 180-188 | Issue | 3 |
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| Publisher | Cambridge University Press (CUP) |
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| URL | |
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| DOI | doi:10.1017/s0885715600011040Search in ResearchGate |
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| Generate Citation Formats |
| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 13253987 | Long-form Identifier | mindat:1:5:13253987:8 |
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| GUID | 0 |
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| Full Reference | Salviulo, Gabriella; Andreozzi, Giovanni B.; Graziani, Giorgio (2000) X-ray characterization of Mg, Fe, and Mn natural end-members of the axinite group. Powder Diffraction, 15 (3). 180-188 doi:10.1017/s0885715600011040 |
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| Plain Text | Salviulo, Gabriella; Andreozzi, Giovanni B.; Graziani, Giorgio (2000) X-ray characterization of Mg, Fe, and Mn natural end-members of the axinite group. Powder Diffraction, 15 (3). 180-188 doi:10.1017/s0885715600011040 |
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| In | (2000, September) Powder Diffraction Vol. 15 (3) Cambridge University Press (CUP) |
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| Abstract/Notes | New powder X-ray diffraction data for magnesio-, ferro-, and manganaxinite, obtained from samples closely corresponding to the three end-members of the axinite mineral group, were obtained using a conventional Bragg–Brentano diffractometer. Space group is P 1¯. Powder patterns were indexed using Peacock's normal orientation, which gave:a=7.1381(3),b=9.1626(4),c=8.9421(4) Å, α=91.903(4), β=98.105(3), γ=77.468(4)° for magnesioaxinite;a=7.1479(4),b=9.1962(5),c=8.9576(4) Å, α=91.857(4), β=98.177(4), γ=77.359(4)° for ferroaxinite, anda=7.1849(4),b=9.2152(5),c=8.9765(4) Å, α=91.761(4), β=98.153(4), γ=77.150(4)° for manganaxinite. Peacock's orientation has been adopted in all recent structural and crystal chemical studies of axinite, but it differs from that reported on the JCPDS cards (29-344, 27-076 and 27-084, respectively). New data include an increased number of indexed peaks. |
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