The diversity of sources of late Archean granites reflects a transition from plume-dominated to plate tectonics in the Superior Province, Canada
[Display omitted] •Late Archean granitic plutons in northeastern Superior Province have diverse sources.•Four granitic suites record transition from plume-dominated regime to plate tectonics.•The ∼2730–2700 Ma subduction-related plutonism is the major crustal growth event.•The transition between tec...
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| Published in | Precambrian research Vol. 370; p. 106525 |
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| Main Authors | , , , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier B.V
01.03.2022
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| Subjects | |
| Online Access | Get full text |
| ISSN | 0301-9268 1872-7433 |
| DOI | 10.1016/j.precamres.2021.106525 |
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| Abstract | [Display omitted]
•Late Archean granitic plutons in northeastern Superior Province have diverse sources.•Four granitic suites record transition from plume-dominated regime to plate tectonics.•The ∼2730–2700 Ma subduction-related plutonism is the major crustal growth event.•The transition between tectonic regimes occurred over a short time span of 30 My.•The transition was markedly diachronous across the Superior Province.
The Superior Province in Canada represents an excellent natural laboratory to test various models of crustal growth and evaluate tectonic regimes during the late Archean. Here, we present new geochemical and geochronological data for ca. 2.8–2.7 Ga plutons intruding different lithotectonic units of the north-eastern part of the Superior Province that demonstrate a complex nature and evolution of magma sources in relation to a changing tectonic setting. Four distinct plutonic suites were newly identified: (1) sodic tonalite–diorite (TD) with a composition resembling low-pressure TTG-like melts, (2) sodic tonalite–granodiorite–diorite (TGD) with medium/high-pressure TTG-like signatures, (3) Mg–K-rich monzogranite to monzodiorite (sanukitoids; MMD), and (4) K-rich granodiorite–granite–monzogranite (GGM). These suites are interpreted as recording a temporal evolution from plume-assisted melting of lower mafic continental crust through melting of a subducted oceanic slab at different depths to large-scale re-melting of the previously formed and amalgamated crustal units. In this evolutionary scheme, the ∼2730–2700 Ma subduction-related plutonism is the most voluminous addition of the juvenile arc material and thus represents the most significant crustal growth event. Altogether, the above inferences and published data suggest that the late Archean plutonism in the Superior Province formed during a transitional regime from plume-dominated to plate-tectonic over a short time span between ∼2730 and ∼2700 Ma and that this transition was markedly diachronous across the Province. |
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| AbstractList | [Display omitted]
•Late Archean granitic plutons in northeastern Superior Province have diverse sources.•Four granitic suites record transition from plume-dominated regime to plate tectonics.•The ∼2730–2700 Ma subduction-related plutonism is the major crustal growth event.•The transition between tectonic regimes occurred over a short time span of 30 My.•The transition was markedly diachronous across the Superior Province.
The Superior Province in Canada represents an excellent natural laboratory to test various models of crustal growth and evaluate tectonic regimes during the late Archean. Here, we present new geochemical and geochronological data for ca. 2.8–2.7 Ga plutons intruding different lithotectonic units of the north-eastern part of the Superior Province that demonstrate a complex nature and evolution of magma sources in relation to a changing tectonic setting. Four distinct plutonic suites were newly identified: (1) sodic tonalite–diorite (TD) with a composition resembling low-pressure TTG-like melts, (2) sodic tonalite–granodiorite–diorite (TGD) with medium/high-pressure TTG-like signatures, (3) Mg–K-rich monzogranite to monzodiorite (sanukitoids; MMD), and (4) K-rich granodiorite–granite–monzogranite (GGM). These suites are interpreted as recording a temporal evolution from plume-assisted melting of lower mafic continental crust through melting of a subducted oceanic slab at different depths to large-scale re-melting of the previously formed and amalgamated crustal units. In this evolutionary scheme, the ∼2730–2700 Ma subduction-related plutonism is the most voluminous addition of the juvenile arc material and thus represents the most significant crustal growth event. Altogether, the above inferences and published data suggest that the late Archean plutonism in the Superior Province formed during a transitional regime from plume-dominated to plate-tectonic over a short time span between ∼2730 and ∼2700 Ma and that this transition was markedly diachronous across the Province. |
| ArticleNumber | 106525 |
| Author | Svojtka, Martin Trubač, Jakub Kachlík, Václav Žák, Jiří Tomek, Filip Vacek, František Sláma, Jiří Santolík, Václav Ackerman, Lukáš Strnad, Ladislav |
| Author_xml | – sequence: 1 givenname: Lukáš surname: Ackerman fullname: Ackerman, Lukáš email: ackerman@gli.cas.cz organization: Institute of Geology of the Czech Academy of Sciences, Rozvojová 269, Prague 6 165 00, Czech Republic – sequence: 2 givenname: Jiří surname: Žák fullname: Žák, Jiří organization: Institute of Geology and Paleontology, Faculty of Science, Charles University, Albertov 6, Prague 128 43, Czech Republic – sequence: 3 givenname: Václav surname: Kachlík fullname: Kachlík, Václav organization: Institute of Geology and Paleontology, Faculty of Science, Charles University, Albertov 6, Prague 128 43, Czech Republic – sequence: 4 givenname: Martin surname: Svojtka fullname: Svojtka, Martin organization: Institute of Geology of the Czech Academy of Sciences, Rozvojová 269, Prague 6 165 00, Czech Republic – sequence: 5 givenname: Filip surname: Tomek fullname: Tomek, Filip organization: Institute of Geology of the Czech Academy of Sciences, Rozvojová 269, Prague 6 165 00, Czech Republic – sequence: 6 givenname: Václav surname: Santolík fullname: Santolík, Václav organization: Institute of Geology of the Czech Academy of Sciences, Rozvojová 269, Prague 6 165 00, Czech Republic – sequence: 7 givenname: Jiří surname: Sláma fullname: Sláma, Jiří organization: Institute of Geology of the Czech Academy of Sciences, Rozvojová 269, Prague 6 165 00, Czech Republic – sequence: 8 givenname: Jakub surname: Trubač fullname: Trubač, Jakub organization: Institute of Geochemistry, Mineralogy and Mineral Resources, Faculty of Science, Charles University, Albertov 6, Prague 128 43, Czech Republic – sequence: 9 givenname: Ladislav surname: Strnad fullname: Strnad, Ladislav organization: Laboratories of the Geological Institutes, Faculty of Science, Charles University, Albertov 6, Prague 128 43, Czech Republic – sequence: 10 givenname: František surname: Vacek fullname: Vacek, František organization: Institute of Geology and Paleontology, Faculty of Science, Charles University, Albertov 6, Prague 128 43, Czech Republic |
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| Keywords | Archean geodynamics Tonalite–trondhjemite–granodiorite (TTG) Superior Province Granite petrogenesis Accretionary orogeny Sr–Nd–Hf |
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| Title | The diversity of sources of late Archean granites reflects a transition from plume-dominated to plate tectonics in the Superior Province, Canada |
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