A geophysical study of the Atlantis-Meteor seamount complex
The depth of the ocean floor in general increases systematically with increasing crustal age (e.g. Sclater and Francheteau, 1970; Parsons and Sclater, 1977). This increase of depth further away from a mid-ocean ridge crest can be explained by thermal models for the evolution of the oceanic lithosphe...
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Other Authors: | , , |
Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
Published: |
Instituut voor Aardwetenschappen RUU
1984
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Online Access: | https://dspace.library.uu.nl/handle/1874/314977 |