Architecture of N orth A tlantic contourite drifts modified by transient circulation of the I celandic mantle plume

Overflow of Northern Component Water, the precursor of North Atlantic Deep Water, appears to have varied during Neogene times. It has been suggested that this variation is moderated by transient behavior of the Icelandic mantle plume, which has influenced North Atlantic bathymetry through time. Thus...

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Veröffentlicht in:	Geochemistry, geophysics, geosystems : G3 geophysics, geosystems : G3, 2015-10, Vol.16 (10), p.3414-3435
Hauptverfasser:	Parnell‐Turner, Ross, White, Nicholas J., McCave, I. Nick, Henstock, Timothy J., Murton, Bramley, Jones, Stephen M.
Format:	Artikel
Sprache:	eng
Online-Zugang:	Volltext
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