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https://hdl.handle.net/2440/13651
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DC Field | Value | Language |
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dc.contributor.author | Wallwork, K. | - |
dc.contributor.author | Pring, A. | - |
dc.contributor.author | Taylor, M. | - |
dc.contributor.author | Hunter, B. | - |
dc.date.issued | 2002 | - |
dc.identifier.citation | Canadian Mineralogist: crystallography, geochemistry, mineralogy, petrology, mineral deposits, 2002; 40(Part 4):1199-1206 | - |
dc.identifier.issn | 0008-4476 | - |
dc.identifier.issn | 1499-1276 | - |
dc.identifier.uri | http://hdl.handle.net/2440/13651 | - |
dc.description.abstract | The crystal structure of priceite, data and refined to Rwp = 0.042 and Rp = 0.030 using the Rietveld method. The monoclinic structure was refined in space group P21/c, a 11.623(1), b 6.976(1), c 12.350(1) Å, β 110.70(1)°, V936.72(1) Å3, Z = 4. The structure consists of infinite chains of pairs of borate rings that extend along [100] via corner-sharing; three corner-linked BΦ4 (Φ: OH-, O2-, or H2O) tetrahedra form one ring linked through a common boron atom to the next ring, composed of two BΦ4 tetrahedra and one BΦ3 triangle. Chains of edge-sharing CaΦ8 polyhedra zigzag along [010]. The borate chains are cross-linked by CaΦ8 polyhedra via edge- and corner-sharing. There are three borates in addition to priceite, that contain a <3B>-<3B> chain motif, but priceite is the only one containing a 3□ ring. These chains extend perpendicular to the calcium chains of polyhedra, in contrast to colemanite, which displays a <3B> motif where the strings are parallel. | - |
dc.language.iso | en | - |
dc.publisher | Mineralogical Assoc Canada | - |
dc.source.uri | http://dx.doi.org/10.2113/gscanmin.40.4.1199 | - |
dc.title | The structure of priceite, a basic hydrated calcium borate, by ab initio powder-diffraction methods | - |
dc.type | Journal article | - |
dc.identifier.doi | 10.2113/gscanmin.40.4.1199 | - |
pubs.publication-status | Published | - |
Appears in Collections: | Aurora harvest 2 Geology & Geophysics publications |
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