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Hodgson, N. A., Le Bas, M. J. (1992) The geochemistry and cryptic zonation of pyrochlore from San Vicente, Cape Verde Islands. Mineralogical Magazine, 56 (383) 201-214 doi:10.1180/minmag.1992.056.383.06

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Reference TypeJournal (article/letter/editorial)
TitleThe geochemistry and cryptic zonation of pyrochlore from San Vicente, Cape Verde Islands
JournalMineralogical MagazineISSN0026-461X
AuthorsHodgson, N. A.Author
Le Bas, M. J.Author
Year1992 (June)Volume56
Issue383
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_56/56-383-201.pdf+
DOIdoi:10.1180/minmag.1992.056.383.06Search in ResearchGate
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Mindat Ref. ID1812Long-form Identifiermindat:1:5:1812:2
GUID0
Full ReferenceHodgson, N. A., Le Bas, M. J. (1992) The geochemistry and cryptic zonation of pyrochlore from San Vicente, Cape Verde Islands. Mineralogical Magazine, 56 (383) 201-214 doi:10.1180/minmag.1992.056.383.06
Plain TextHodgson, N. A., Le Bas, M. J. (1992) The geochemistry and cryptic zonation of pyrochlore from San Vicente, Cape Verde Islands. Mineralogical Magazine, 56 (383) 201-214 doi:10.1180/minmag.1992.056.383.06
In(1992, June) Mineralogical Magazine Vol. 56 (383) Mineralogical Society
Abstract/NotesAbstractZr-rich pyrochlore crystals in carbonatite from San Vicente (Cape Verdes Islands) show cryptic, concentric and rhythmic chemical zonation with Ca increasing and Ti, U and Zr decreasing towards the rims. In one carbonatite, taken from the Camile dyke, previously undocumented cryptic sector zonation of Ti, U and Zr is also observed in these crystals. The chemical variation is investigated by wavelength-dispersive electron microprobe, with both single spot and crystal map analyses.The concentric and rhythmic zonation, marked by element substitution, was generated by magma heterogeneity and/or element diffusion kinetics, but it is suggested that the sector zonation, marked by differential site substitution, was governed by protosite variation between octahedral and cubic faces.


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