Abstract
Estimates of the relative motion between the Hawaiian and Louisville hot spots have consequences for understanding the role and character of deep Pacific-mantle return flow. The relative motion between these primary hot spots can be inferred by comparing the age records for their seamount trails. We report
Original language | English |
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Article number | 10 |
Pages (from-to) | 4564-4584 |
Journal | Geochemistry, Geophysics, Geosystems |
Issue number | 14 |
DOIs | |
Publication status | Published - 2013 |