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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Bibliographic Details
Main Author: Verhoef, J.
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: 1984
Subjects:
Online Access:https://dspace.library.uu.nl/handle/1874/238521