Paleomagnetic direction and paleointensity variations during the Matuyama–Brunhes polarity transition from a marine succession in the Chiba composite section of the Boso Peninsula, central Japan
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DOI: 10.1186/s40623-017-0627-1
Abstract: The youngest geomagnetic polarity reversal, the Matuyama–Brunhes (M–B) boundary, provides an important plane of data for sediments, ice cores, and lavas. The geomagnetic field intensity and directional changes that occurred during the reversal also provide… read more here.
Keywords: paleointensity; composite section; polarity; matuyama brunhes ... See more keywords