Paleomagnetic inclination variations during the last 200 kyr in the Okhotsk Sea and their relation to persistent non-axial-dipole field
Author:
Funder
Japan Society for the Promotion of Science
Publisher
Springer Science and Business Media LLC
Subject
Space and Planetary Science,Geology
Link
http://link.springer.com/content/pdf/10.1186/s40623-016-0561-7.pdf
Reference25 articles.
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3. Guyodo Y, Valet J-P (1999) Global changes in intensity of the Earth’s magnetic field during the past 800 kyr. Nature 399:249–252
4. Hoffman KA, Singer BS (2008) Magnetic source separation in Earth’s outer core. Science 321:1800
5. Inoue S, Yamazaki T (2010) Geomagnetic relative paleointensity chronostratigraphy of sediment cores from the Okhotsk Sea. Palaeogeogr Palaeoclimatol Palaeoecol 291:253–266
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