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dc.contributor.authorFinch, A. A.
dc.contributor.authorGoodenough, K M
dc.contributor.authorSalmon, H M
dc.contributor.authorAndersen, T
dc.date.accessioned2019-02-07T16:30:04Z
dc.date.available2019-02-07T16:30:04Z
dc.date.issued2001-12
dc.identifier786481
dc.identifier91d7dc41-4864-43fa-8b9e-a510c83663d9
dc.identifier000172705200007
dc.identifier0035655636
dc.identifier.citationFinch , A A , Goodenough , K M , Salmon , H M & Andersen , T 2001 , ' The petrology and petrogenesis of the North Motzfeldt Centre, Gardar Province, South Greenland ' , Mineralogical Magazine , vol. 65 , no. 6 , pp. 759-774 . https://doi.org/10.1180/0026461016560007en
dc.identifier.issn0026-461X
dc.identifier.otherORCID: /0000-0002-3689-1517/work/53857082
dc.identifier.urihttps://hdl.handle.net/10023/17016
dc.descriptionThe Carnegie Trust for the Universities of Scotland, The Percy Sladen Trust, The Royal Geographical Society, The Mineralogical Society of Great Britain and Ireland, NERC and the University of Luton gave financial assistance for the present study. Radiometric studies formed part of a collaborative programme between AAF and TA funded by the British Council.en
dc.description.abstractNorth Motzfeldt is an intrusive igneous centre within the Igaliku (formerly spelt Igaliko) complex, Gardar Province, South Greenland. A detailed field description of the centre is given, with preliminary geochemical and isotopic data. The North Motzfeldt centre is intruded into Ketilidian granitoid basement rocks, and current exposure retains parts of the original roof against earlier Gardar eruptives and elastic sediments of the Eriksfjord formation. The unconformity between the Ketilidian and the overlying Eriksfjord is believed to have been crucial in the siting of the centre. The centre is subdivided into two major units, NM1 and NM2. This was followed by significant peralkaline nepheline microsyenite in sheets, characterized by rare element-rich accessory minerals including rinkite-mosandrite, pyrochlore and lavenite. A significant microsyenite body is called NM3. A preliminary Rb-Sr isochron of 1226 +/- 27 Ma indicates a far younger age for the centre than previously thought (similar to 1350 Ma). Cross-cutting relationships between North Motzfeldt and rocks of the adjacent Motzfeldt centre require a reappraisal of the chronology of Motzfeldt magmatism. We suggest that rocks previously believed to comprise the Motzfeldt centre represent the products of multiple phases of magmatism from Early- to Mid-Gardar times.
dc.format.extent16
dc.format.extent767308
dc.language.isoeng
dc.relation.ispartofMineralogical Magazineen
dc.subjectGardaren
dc.subjectKetilidianen
dc.subjectNepheline syeniteen
dc.subjectMagma chamberen
dc.subjectRoof zonesen
dc.subjectQE Geologyen
dc.subject.lccQEen
dc.titleThe petrology and petrogenesis of the North Motzfeldt Centre, Gardar Province, South Greenlanden
dc.typeJournal articleen
dc.contributor.institutionUniversity of St Andrews. School of Earth & Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews. Scottish Oceans Instituteen
dc.contributor.institutionUniversity of St Andrews. St Andrews Isotope Geochemistryen
dc.identifier.doi10.1180/0026461016560007
dc.description.statusPeer revieweden
dc.date.embargoedUntil2002-12-01


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