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Braithwaite, R. S. W. (1983) Infrared spectroscopic analysis of the olivenite-adamite series, and of phosphate substitution in olivenite. Mineralogical Magazine, 47 (342) 51-57 doi:10.1180/minmag.1983.047.342.09

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Reference TypeJournal (article/letter/editorial)
TitleInfrared spectroscopic analysis of the olivenite-adamite series, and of phosphate substitution in olivenite
JournalMineralogical MagazineISSN0026-461X
AuthorsBraithwaite, R. S. W.Author
Year1983 (March)Volume47
Issue342
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_47/47-342-51.pdf+
DOIdoi:10.1180/minmag.1983.047.342.09Search in ResearchGate
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Mindat Ref. ID3471Long-form Identifiermindat:1:5:3471:9
GUID0
Full ReferenceBraithwaite, R. S. W. (1983) Infrared spectroscopic analysis of the olivenite-adamite series, and of phosphate substitution in olivenite. Mineralogical Magazine, 47 (342) 51-57 doi:10.1180/minmag.1983.047.342.09
Plain TextBraithwaite, R. S. W. (1983) Infrared spectroscopic analysis of the olivenite-adamite series, and of phosphate substitution in olivenite. Mineralogical Magazine, 47 (342) 51-57 doi:10.1180/minmag.1983.047.342.09
In(1983, March) Mineralogical Magazine Vol. 47 (342) Mineralogical Society
Abstract/NotesAbstractInfrared spectroscopy affords a rapid and easy method of estimating the position of a mineral in the olivenite-adamite solid solution series, and of estimating the amount of phosphate substitution in olivenites. Toman's discovery of the monoclinic symmetry of olivenites with up to approximately 20 atom % Zn/(Cu + Zn) has raised a problem in nomenclature. It is suggested that the definition of ‘cuproadamite’ be extended to cover all orthorhombic members of the series containing appreciable Cu. Studies of deuterated materials have helped to solve some of the absorption band assignments for olivenite-adamite, libethenite and related minerals.

Mineral Pages

MineralCitation Details
Adamite-Olivenite Series
Libethenite-Olivenite Series
Olivenite
Zincolivenite


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