Changes in position and intensity of Deep Western Boundary Current during the late Pleistocene (Marine Isotope Stages 8-10) inferred from grain size of Northwest Atlantic sediment drifts(abs.)

Authors=YOKOKAWA Miwa, FRANZ Sven-O.

Journal/Book_names=Program and Abstracts, Annual Meeting of the Sedimentological Society of Japan

volume=2002

pages=9-10

Publish_year=2002

Publish_Country=JPN

Publisher=Sedimentological Society of Japan

Language_of_Text=JA

ID=200650698