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Gilkes, R. J., Palmer, B. (1983) Synthesis, properties, and dehydroxylation of members of the crandallite-goyazite series. Mineralogical Magazine, 47 (343) 221-227 doi:10.1180/minmag.1983.047.343.13

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Reference TypeJournal (article/letter/editorial)
TitleSynthesis, properties, and dehydroxylation of members of the crandallite-goyazite series
JournalMineralogical MagazineISSN0026-461X
AuthorsGilkes, R. J.Author
Palmer, B.Author
Year1983 (June)Volume47
Issue343
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_47/47-343-221.pdf+
DOIdoi:10.1180/minmag.1983.047.343.13Search in ResearchGate
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Mindat Ref. ID3503Long-form Identifiermindat:1:5:3503:7
GUID0
Full ReferenceGilkes, R. J., Palmer, B. (1983) Synthesis, properties, and dehydroxylation of members of the crandallite-goyazite series. Mineralogical Magazine, 47 (343) 221-227 doi:10.1180/minmag.1983.047.343.13
Plain TextGilkes, R. J., Palmer, B. (1983) Synthesis, properties, and dehydroxylation of members of the crandallite-goyazite series. Mineralogical Magazine, 47 (343) 221-227 doi:10.1180/minmag.1983.047.343.13
In(1983, June) Mineralogical Magazine Vol. 47 (343) Mineralogical Society
Abstract/NotesAbstractUnit-cell parameters of synthesized members of the crandallite (a = 7.007 Å, c = 16.216 Å)-goyazite (a = 7.013 Å, c = 16.650 Å) series vary linearly with composition between end-members. Most members of the series consist of 0.1 μm platy crystals, but crandallite also contains some larger (1–5 µm) tapered crystals elongated along the c axis.With increasing Sr substitution the dehydroxylation temperature decreases from c. 475 °C for crandallite to 420 °C at 20 mole % Sr, and then increases to 440 °C for goyazite. Partial dehydroxylation of crandallite is accompanied by contraction of the c unit cell parameter and expansion of a, thereby retaining an unaltered unit cell volume. The much greater sensitivity of c to both Sr substitution and dehydroxylation may be due to the rigidity of continuous sheets of Al(OH)4O2 octahedra which are parallel to the (001) plane in these minerals.

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MineralCitation Details
Crandallite
Goyazite


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