Earth's magnetic field: ocean current contributions to vertical profiles in deep oceans
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Lilley, F. E. M.
White, A.
Heinson, Graham
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Blackwell Publishing Ltd
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The Earth's main magnetic field, arising in the core, should, in the ocean, have a well-defined uniform gradient with depth. Superimposed upon this uniform gradient may be magnetic signals due to a variety of sources. These include crustal magnetization,
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Geophysical Journal International
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Restricted until
2037-12-31
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