Changes in grain size and magnetic fabric at Blake–Bahama Outer Ridge during the late Pleistocene (marine isotope stages 8–10)

ODP Sites 1055–1062 on the Blake-Bahama Outer Ridge (BBOR) are characterized by high sedimentation rates, which allow high-resolution analyses to reconstruct the behavior of the Deep Western Boundary Current (DWBC) as a function of depth along the BBOR. The ODP sites provide an intermediate and deep...

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Veröffentlicht in:	Marine geology 2002-09, Vol.189 (1), p.123-144
Hauptverfasser:	Yokokawa, Miwa, Franz, Sven-Oliver
Format:	Artikel
Sprache:	eng
Schlagworte:	anisotropy of magnetic susceptibility Blake–Bahama Outer Ridge Deep Western Boundary Current grain size late Pleistocene Marine Ocean Drilling Program
Online-Zugang:	Volltext
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