Scientific drilling in the South Atlantic: International Ocean Discovery Program Workshop; Rio de Janeiro, Brazil, 2-5 April 201

The South Atlantic is a classic example of continental breakup in which the mechanisms that drove the initial fragmentation still need to be detailed. Mantle plumes may have played a key role in this process, as implied by the Rio Grande Rise (RGR) and Walvis Ridge (WR) hot spot tracks. Their role i...

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Hauptverfasser: Santos, Roberto Ventura (VerfasserIn) , Glasmacher, Ulrich A. (VerfasserIn) , Geldmacher, Jörg (VerfasserIn)
Dokumenttyp: Article (Journal) Konferenzschrift
Sprache:Englisch
Veröffentlicht: 8 July 2014
In: Eos
Year: 2014, Jahrgang: 95, Heft: 27, Pages: 249-249
ISSN:2324-9250
DOI:https://doi.org/10.1002/2014EO270007
Online-Zugang:Verlag, lizenzpflichtig, Volltext: https://doi.org/https://doi.org/10.1002/2014EO270007
Verlag, lizenzpflichtig, Volltext: https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1002/2014EO270007
Volltext
Verfasserangaben:Roberto Ventura Santos, Ulrich A. Glasmacher, and Jörg Geldmacher
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Zusammenfassung:The South Atlantic is a classic example of continental breakup in which the mechanisms that drove the initial fragmentation still need to be detailed. Mantle plumes may have played a key role in this process, as implied by the Rio Grande Rise (RGR) and Walvis Ridge (WR) hot spot tracks. Their role in the South Atlantic opening is uncertain, as questions remain about their origin and relationship with the structure and dynamics of the upper mantle. Recent findings indicate that the western margin of continental South America did not behave as a rigid block but instead stretched significantly, allowing the emplacement of igneous and exhumed mantle rocks. Continental rifting may have rafted fragments of the continents into the ocean, as implied by recently dredged continental rocks from the RGR.
Beschreibung:Gesehen am 21.01.2021
Beschreibung:Online Resource
ISSN:2324-9250
DOI:https://doi.org/10.1002/2014EO270007