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Thesis

Tectonics of the western Mediterranean

Abstract:

The evolution of the Western Mediterranean takes place between the converging African and Eurasian plates, therefore the motion between them cannot be determined directly. The motion between them is the finite difference between the independent seafloor spreading systems in the Central and North Atlantic Oceans.

Primary magnetic anomaly data from the North and Central Atlantic was reexamined. All Late Cretaceous and Cenozoic anomalies (Anomaly 34 - Anomaly 2) were remapped. Fractur...

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Institution:
University of Oxford
Department:
Mathematical and Physical Sciences Division

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Publication date:
1989
Type of award:
DPhil
Level of award:
Doctoral
Awarding institution:
University of Oxford
Barcode:
602819950
URN:
uuid:8d799ab4-d55f-4f58-92a6-1478dd14e5f3
Local pid:
td:602819950
Language:
English
Subjects:

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