Seafloor spreading pattern of the North Atlantic between 10⁰ and 40⁰ N: a reconstruction based on shipborne measurements and satellite altimeter data
The history of the relative motion between North America and Africa is recorded in the floor of the central North Atlantic Ocean. The resulting pattern of magnetic anomalies and fracture zones in the area between 10° and 40° N was analysed using shipborne measurements and Seasat altimeter data. This...
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Other Authors: | , , |
Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
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Faculteit Aardwetenschappen
1987
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Online Access: | https://dspace.library.uu.nl/handle/1874/315937 |