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Uitterdijk Appel, Peter W. (1997) Al-rich warwickite from lnglefield Land, North-West Greenland. Mineralogical Magazine, 61 (408) 693-698 doi:10.1180/minmag.1997.061.408.08

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Reference TypeJournal (article/letter/editorial)
TitleAl-rich warwickite from lnglefield Land, North-West Greenland
JournalMineralogical MagazineISSN0026-461X
AuthorsUitterdijk Appel, Peter W.Author
Year1997 (October)Volume61
Page(s)693-698Issue408
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_61/61-408-693.pdf+
DOIdoi:10.1180/minmag.1997.061.408.08Search in ResearchGate
Mindat Ref. ID208Long-form Identifiermindat:1:5:208:4
GUID413c0f3c-0160-411c-a20a-8e4e33dbe6bb
Full ReferenceUitterdijk Appel, Peter W. (1997) Al-rich warwickite from lnglefield Land, North-West Greenland. Mineralogical Magazine, 61 (408) 693-698 doi:10.1180/minmag.1997.061.408.08
Plain TextUitterdijk Appel, Peter W. (1997) Al-rich warwickite from lnglefield Land, North-West Greenland. Mineralogical Magazine, 61 (408) 693-698 doi:10.1180/minmag.1997.061.408.08
In(1997, October) Mineralogical Magazine Vol. 61 (408) Mineralogical Society
Abstract/NotesAbstractWarwickite constitutes about 5% of an outcrop of metamorphosed ultramafic rocks of Precambrian age in North-West Greenland. It occurs as slender grains, several millimetres long, and in anhedral grains up to 5 mm in size, together with forsterite, pleonaste, phlogopite, magnetite ± tourmaline. Post-metamorphic alteration of warwickite produced a network of boron-rich minerals and magnetite. The warwickite, containing up to 9.72% Al2O3, displays a significantly different chemical composition from warwickite elsewhere, such as that in recrystallized limestones from the type locality Warwick, New York, and in lamproitic and carbonatite-like rocks at Jumilla, Spain.


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