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
| 形式 | 参考書籍・資料 |
|---|---|
| 著者 | 岡田誠, 菅沼悠介, 羽田裕貴, 風岡修 |
| オンライン版公開日 | 2017年3月21日 |
| 掲載誌 | Earth, Planets and Space |
購入先
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 important information for understanding the dynamics of the Earth’s outer core, which generates the magnetic field.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 | Earth, Planets and Space | Full Text
