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Schönenberger, J., Markl, G. (2008) The Magmatic and Fluid Evolution of the Motzfeldt Intrusion in South Greenland: Insights into the Formation of Agpaitic and Miaskitic Rocks. Journal of Petrology, 49 (9) 1549-1577 doi:10.1093/petrology/egn037

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Reference TypeJournal (article/letter/editorial)
TitleThe Magmatic and Fluid Evolution of the Motzfeldt Intrusion in South Greenland: Insights into the Formation of Agpaitic and Miaskitic Rocks
JournalJournal of Petrology
AuthorsSchönenberger, J.Author
Markl, G.Author
Year2008 (August 2)Volume<   49   >
Issue<   9   >
PublisherOxford University Press (OUP)
URL
DOIdoi:10.1093/petrology/egn037Search in ResearchGate
Generate Citation Formats
Original EntrySchönenberger J. & Markl G.(2008).The magmatic and fluid evolution of the Motzfeldt intrusion in South Greenland: insights into the formation of agpaitic and miaskitic rocks.Journal of Petrology 49(9) 1549-1577.
Classification
Not set
LoC
Not set
Mindat Ref. ID16058430Long-form Identifiermindat:1:5:16058430:7
GUID0
Full ReferenceSchönenberger, J., Markl, G. (2008) The Magmatic and Fluid Evolution of the Motzfeldt Intrusion in South Greenland: Insights into the Formation of Agpaitic and Miaskitic Rocks. Journal of Petrology, 49 (9) 1549-1577 doi:10.1093/petrology/egn037
Plain TextSchönenberger, J., Markl, G. (2008) The Magmatic and Fluid Evolution of the Motzfeldt Intrusion in South Greenland: Insights into the Formation of Agpaitic and Miaskitic Rocks. Journal of Petrology, 49 (9) 1549-1577 doi:10.1093/petrology/egn037
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Locality Pages

LocalityCitation Details
Motzfeldt Centre, Igaliku Complex, Kujalleq, Greenland

Mineral Occurrences

LocalityMineral(s)
Motzfeldt Centre, Igaliku Complex, Kujalleq, Greenland Aegirine, Arfvedsonite, Diopside, Eudialyte, Fayalite-Forsterite Series, Ferro-ferri-katophorite, Ferro-nybøite, Ferro-richterite, Fluorite, Hastingsite, Hedenbergite, Hematite, Ilmenite, Magnesio-hastingsite, Magnetite, Nepheline, Pargasite, Potassic-arfvedsonite, Riebeckite, Taramite, Titanium-bearing Magnetite, Zircon


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