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Contiguous Laurenti...
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Romer, RolfLuleå tekniska universitet
(author)
Contiguous Laurentia and Baltica before the Grenvillian-Sveconorwegian orogeny?
- Article/chapterEnglish1996
Publisher, publication year, extent ...
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Wiley,1996
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printrdacarrier
Numbers
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LIBRIS-ID:oai:DiVA.org:ltu-8542
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https://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-8542URI
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https://doi.org/10.1111/j.1365-3121.1996.tb00741.xDOI
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Language:English
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Summary in:English
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Subject category:ref swepub-contenttype
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Subject category:art swepub-publicationtype
Notes
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Godkänd; 1996; 20080527 (cira)
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Close geochronological correspondence of Mesoproterozoic extension-related magmatism and comparable tectonic and geochronological evolution of the Grenville and Svecononvegian orogens suggests that the Laurentian and Baltic Shields could have been joined during the Mesoproterozoic and did not separate until after the Grenvillian-Sveconorwegian orogeny. The combined Grenville-Svecononvegian orogen is here interpreted to have formed during the collision of coherent Laurentia-Baltica with an unknown craton, which is in contrast to earlier explanations that favour a late-Mesoproterozoic rotation between Laurentia and Baltica followed by collision of these two cratons with each other
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Luleå tekniska universitet
(creator_code:org_t)
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In:Terra Nova: Wiley8:2, s. 173-1810954-48791365-3121
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