Lead Isotopes and the Sources of Granitic Magmas: The Sveconorwegian Granite and Pegmatite Province of Southern Norway

Lead isotope analyses of K-feldspar from late Sveconorwegian (900–1000 Ma) granitic pegmatites and A-type, ferroan granitic intrusions in four different areas of southern Norway analyzed by laser-ablation inductively coupled plasma source mass spectrometry (LA-ICPMS) give compositions in the range &...
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Autor*in:	Nanna Rosing-Schow [verfasserIn] Tom Andersen [verfasserIn] Axel Müller [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2022

Schlagwörter:	granites pegmatites Pb isotopes source modelling Sveconorwegian orogen southern Norway

Übergeordnetes Werk:	In: Minerals - MDPI AG, 2012, 12(2022), 7, p 878
Übergeordnetes Werk:	volume:12 ; year:2022 ; number:7, p 878

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/min12070878

Katalog-ID:	DOAJ035932759

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520			\|a Lead isotope analyses of K-feldspar from late Sveconorwegian (900–1000 Ma) granitic pegmatites and A-type, ferroan granitic intrusions in four different areas of southern Norway analyzed by laser-ablation inductively coupled plasma source mass spectrometry (LA-ICPMS) give compositions in the range <sup<206</sup<Pb/<sup<204</sup<Pb = 16.637 to 17.555, <sup<207</sup<Pb/<sup<204</sup<Pb = 15.445 to 15.534, <sup<208</sup<Pb/<sup<204</sup<Pb = 36.317 to 37.459. These compositions broadly overlap with the initial compositions estimated from previously published solution TIMS whole-rock and feldspar Pb isotope analyses of late Sveconorwegian granitic plutons across the region, suggesting that magmas forming A-type granite plutons and granitic pegmatites have been derived from broadly similar source rocks, i.e., from a continental crust that initially formed in Palaeoproterozoic time (ca. 2.10–1.86 Ga), and subsequently underwent intracrustal partial melting, differentiation and rejuvenation via mafic underplating in Mesoproterozoic time.
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author	Nanna Rosing-Schow
spellingShingle	Nanna Rosing-Schow misc QE351-399.2 misc granites misc pegmatites misc Pb isotopes misc source modelling misc Sveconorwegian orogen misc southern Norway misc Mineralogy Lead Isotopes and the Sources of Granitic Magmas: The Sveconorwegian Granite and Pegmatite Province of Southern Norway
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topic_title	QE351-399.2 Lead Isotopes and the Sources of Granitic Magmas: The Sveconorwegian Granite and Pegmatite Province of Southern Norway granites pegmatites Pb isotopes source modelling Sveconorwegian orogen southern Norway
topic	misc QE351-399.2 misc granites misc pegmatites misc Pb isotopes misc source modelling misc Sveconorwegian orogen misc southern Norway misc Mineralogy
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title	Lead Isotopes and the Sources of Granitic Magmas: The Sveconorwegian Granite and Pegmatite Province of Southern Norway
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title_full	Lead Isotopes and the Sources of Granitic Magmas: The Sveconorwegian Granite and Pegmatite Province of Southern Norway
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title_sort	lead isotopes and the sources of granitic magmas: the sveconorwegian granite and pegmatite province of southern norway
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title_auth	Lead Isotopes and the Sources of Granitic Magmas: The Sveconorwegian Granite and Pegmatite Province of Southern Norway
abstract	Lead isotope analyses of K-feldspar from late Sveconorwegian (900–1000 Ma) granitic pegmatites and A-type, ferroan granitic intrusions in four different areas of southern Norway analyzed by laser-ablation inductively coupled plasma source mass spectrometry (LA-ICPMS) give compositions in the range <sup<206</sup<Pb/<sup<204</sup<Pb = 16.637 to 17.555, <sup<207</sup<Pb/<sup<204</sup<Pb = 15.445 to 15.534, <sup<208</sup<Pb/<sup<204</sup<Pb = 36.317 to 37.459. These compositions broadly overlap with the initial compositions estimated from previously published solution TIMS whole-rock and feldspar Pb isotope analyses of late Sveconorwegian granitic plutons across the region, suggesting that magmas forming A-type granite plutons and granitic pegmatites have been derived from broadly similar source rocks, i.e., from a continental crust that initially formed in Palaeoproterozoic time (ca. 2.10–1.86 Ga), and subsequently underwent intracrustal partial melting, differentiation and rejuvenation via mafic underplating in Mesoproterozoic time.
abstractGer	Lead isotope analyses of K-feldspar from late Sveconorwegian (900–1000 Ma) granitic pegmatites and A-type, ferroan granitic intrusions in four different areas of southern Norway analyzed by laser-ablation inductively coupled plasma source mass spectrometry (LA-ICPMS) give compositions in the range <sup<206</sup<Pb/<sup<204</sup<Pb = 16.637 to 17.555, <sup<207</sup<Pb/<sup<204</sup<Pb = 15.445 to 15.534, <sup<208</sup<Pb/<sup<204</sup<Pb = 36.317 to 37.459. These compositions broadly overlap with the initial compositions estimated from previously published solution TIMS whole-rock and feldspar Pb isotope analyses of late Sveconorwegian granitic plutons across the region, suggesting that magmas forming A-type granite plutons and granitic pegmatites have been derived from broadly similar source rocks, i.e., from a continental crust that initially formed in Palaeoproterozoic time (ca. 2.10–1.86 Ga), and subsequently underwent intracrustal partial melting, differentiation and rejuvenation via mafic underplating in Mesoproterozoic time.
abstract_unstemmed	Lead isotope analyses of K-feldspar from late Sveconorwegian (900–1000 Ma) granitic pegmatites and A-type, ferroan granitic intrusions in four different areas of southern Norway analyzed by laser-ablation inductively coupled plasma source mass spectrometry (LA-ICPMS) give compositions in the range <sup<206</sup<Pb/<sup<204</sup<Pb = 16.637 to 17.555, <sup<207</sup<Pb/<sup<204</sup<Pb = 15.445 to 15.534, <sup<208</sup<Pb/<sup<204</sup<Pb = 36.317 to 37.459. These compositions broadly overlap with the initial compositions estimated from previously published solution TIMS whole-rock and feldspar Pb isotope analyses of late Sveconorwegian granitic plutons across the region, suggesting that magmas forming A-type granite plutons and granitic pegmatites have been derived from broadly similar source rocks, i.e., from a continental crust that initially formed in Palaeoproterozoic time (ca. 2.10–1.86 Ga), and subsequently underwent intracrustal partial melting, differentiation and rejuvenation via mafic underplating in Mesoproterozoic time.
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title_short	Lead Isotopes and the Sources of Granitic Magmas: The Sveconorwegian Granite and Pegmatite Province of Southern Norway
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Lead Isotopes and the Sources of Granitic Magmas: The Sveconorwegian Granite and Pegmatite Province of Southern Norway

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