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Rock magnetic properties of the Gardar Drift sedimentary sequence, Site IODP U1314, North Atlantic: Implications for bottom current change through the mid-Pleistocene
 

Summary: Rock magnetic properties of the Gardar Drift sedimentary sequence, Site IODP U1314,
North Atlantic: Implications for bottom current change through the mid-Pleistocene
T. Kanamatsu a,
, M. Ohno b
, G. Acton c
, H. Evans d
, Y. Guyodo e
a
Institute for Research on Earth Evolution (IFREE), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka 237-0061, Japan
b
Department of Environmental Changes, Faculty of Social and Cultural Studies, Kyushu University, 744 Motooka, Nishi-ku, Fukuoka, 819-0395 Japan
c
Department of Geology, University of California, Davis One Shields Avenue Davis, CA 95616 USA
d
Lamont-Doherty Earth Observatory of Columbia University PO Box 1000, 61 Route 9 W Palisades NY 10964 USA
e
Institut de Mineralogie et de Physique des Milieux CondensÚs (IMPMC, UMR 7590 CNRS/UPMC/UPD/IPGP), 140 rue de Lourmel, 75015 Paris, France
a b s t r a c ta r t i c l e i n f o
Article history:
Received 7 May 2008

  

Source: Acton, Gary - Department of Geology, University of California, Davis

 

Collections: Geosciences