Preliminary report on the relative paleointensity variation during the Eocene deduced from the IODP Sites U1403 and U1408 marine sediments recovered from the northwest Atlantic

Yuhji Yamamoto1, Hiroto Fukami2,3, Wakana Taniguchi2 and Peter C Lippert4, (1)Kochi University, Center for Advanced Marine Core Research, Kochi, Japan, (2)Kochi University, Kochi, Japan, (3)Sanyo Techno Marine Co., Ltd., Tokyo, Japan, (4)University of Utah, Department of Geology and Geophysics, Salt Lake City, UT, United States