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Earth's magnetic field: ocean current contributions to vertical profiles in deep oceans

Lilley, F. E. M.; White, A.; Heinson, Graham


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,

CollectionsANU Research Publications
Date published: 2001
Type: Journal article
Source: Geophysical Journal International
DOI: 10.1046/j.1365-246X.2001.00514.x


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