| Reference Type | Journal (article/letter/editorial) |
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| Title | Al-rich warwickite from lnglefield Land, North-West Greenland |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Uitterdijk Appel, Peter W. | Author |
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| Year | 1997 (October) | Volume | 61 |
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| Issue | 408 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_61/61-408-693.pdf+ |
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| DOI | doi:10.1180/minmag.1997.061.408.08Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 208 | Long-form Identifier | mindat:1:5:208:4 |
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| GUID | 0 |
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| Full Reference | 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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| Plain Text | 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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| In | (1997, October) Mineralogical Magazine Vol. 61 (408) Mineralogical Society |
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| Abstract/Notes | AbstractWarwickite 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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