ON GEOID HEIGHTS AND FLEXURE OF THE LITHOSPHERE AT SEAMOUNTS
Preliminary studies have been carried out of how oceanic volcanoes, which rise above the ocean floor as isolated seamounts and oceanic islands or linear ridges, contribute to the marine geoid. Simple 1- and 2-D models have been constructed in which it is assumed that the oceanic lithosphere responds...
| Main Authors: | , |
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| Format: | Journal article |
| Language: | English |
| Published: |
1984
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