Magnetism and Opaque Mineralogy of Basalts from the Mid-Atlantic Ridge at 45° N
The volcanic layer may be only 200 m thick at 45° N and oxidation of titanomagnetite may be responsible for the decrease in amplitude of the magnetic anomalies away from the ridge axis.
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| Veröffentlicht in: | Nature (London) 1970-12, Vol.228 (5275), p.974-976 |
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| container_end_page | 976 |
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| container_issue | 5275 |
| container_start_page | 974 |
| container_title | Nature (London) |
| container_volume | 228 |
| creator | IRVING, E PARK, J. K HAGGERTY, S. E AUMENTO, F LONCAREVIC, B |
| description | The volcanic layer may be only 200 m thick at 45° N and oxidation of titanomagnetite may be responsible for the decrease in amplitude of the magnetic anomalies away from the ridge axis. |
| doi_str_mv | 10.1038/228974a0 |
| format | Article |
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| ispartof | Nature (London), 1970-12, Vol.228 (5275), p.974-976 |
| issn | 0028-0836 1476-4687 |
| language | eng |
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| source | Nature; SpringerLink Journals - AutoHoldings |
| subjects | Humanities and Social Sciences multidisciplinary Science Science (multidisciplinary) |
| title | Magnetism and Opaque Mineralogy of Basalts from the Mid-Atlantic Ridge at 45° N |
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