Mellini, M., Cressey, G., Wicks, F. J., Cressey, B. A. (2010) The crystal structure of Mg end-member lizardite-1T forming polyhedral spheres from the Lizard, Cornwall. Mineralogical Magazine, 74 (2) 277-284 doi:10.1180/minmag.2010.074.2.277
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | The crystal structure of Mg end-member lizardite-1T forming polyhedral spheres from the Lizard, Cornwall | ||
| Journal | Mineralogical Magazine | ||
| Authors | Mellini, M. | Author | |
| Cressey, G. | Author | ||
| Wicks, F. J. | Author | ||
| Cressey, B. A. | Author | ||
| Year | 2010 (April) | Volume | 74 |
| Issue | 2 | ||
| Publisher | Mineralogical Society | ||
| DOI | doi:10.1180/minmag.2010.074.2.277Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 244067 | Long-form Identifier | mindat:1:5:244067:9 |
| GUID | 0 | ||
| Full Reference | Mellini, M., Cressey, G., Wicks, F. J., Cressey, B. A. (2010) The crystal structure of Mg end-member lizardite-1T forming polyhedral spheres from the Lizard, Cornwall. Mineralogical Magazine, 74 (2) 277-284 doi:10.1180/minmag.2010.074.2.277 | ||
| Plain Text | Mellini, M., Cressey, G., Wicks, F. J., Cressey, B. A. (2010) The crystal structure of Mg end-member lizardite-1T forming polyhedral spheres from the Lizard, Cornwall. Mineralogical Magazine, 74 (2) 277-284 doi:10.1180/minmag.2010.074.2.277 | ||
| In | (2010, April) Mineralogical Magazine Vol. 74 (2) Mineralogical Society | ||
| Abstract/Notes | AbstractThe crystal structure of lizardite-1T from Gew-graze, Cornwall, has been refined by single-crystal X-ray diffraction to R1 of 0.0263 and 0.0557, for two crystals having P31m space group and lattice parameters a = 5.2905(5) Å, c = 7.2815(8) Å, and a = 5.3111(10) Å, c = 7.2907(15) Å, respectively. The Gew-graze lizardite is very close to the end-member composition, so these refinements confirm the existence of well crystallized pure Mg-lizardite and show this to be the most weakly H-bonded lizardite ever refined. With regard to its lattice parameters, Si–O bond distances and geometrical parameters controlled by interlayer interactions (i.e. H-bonding), the Gew-graze Mg end-member lizardite yields slight but observable geometrical differences compared with previous refined structures for specifically, aluminous, lizardites. | ||
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