Un “fit” structural de l'Atlantique Nord: Arguments geologiques pour correler les marqueurs geophysiques reconnus sur les deux marges
- 1 September 1980
- journal article
- Published by Elsevier in Marine Geology
- Vol. 37 (3-4) , 355-369
- https://doi.org/10.1016/0025-3227(80)90110-3
Abstract
No abstract availableKeywords
This publication has 50 references indexed in Scilit:
- Les decrochements tardi-hercyniens du sud-ouest de l'europe. Geometrie et essai de reconstitution des conditions de la deformationPublished by Elsevier ,2003
- The Newport granite: its age, geological setting, and implications for the geology of northeastern NewfoundlandCanadian Journal of Earth Sciences, 1979
- Geologie du plateau continental sud-armoricain entre les iles de Glenan et de Noirmoutier; implications geodynamiquesBSGF - Earth Sciences Bulletin, 1977
- The Gander–Avalon Zone boundary in southeastern NewfoundlandCanadian Journal of Earth Sciences, 1976
- Age relationships along the Hermitage Bay–Dover Fault System, NewfoundlandNature, 1976
- Evidence for the Emergence of the Hercynian Front on the North American ContinentCanadian Journal of Earth Sciences, 1975
- Geomagnetic reconnaissance on the continental margin of the British Isles between 54° and 57° NJournal of the Geological Society, 1975
- The Dover Fault: Western Boundary of the Avalon Zone in Northeastern NewfoundlandCanadian Journal of Earth Sciences, 1975
- Is the Gibbs Fracture Zone a Westward Projection of the Hercynian Front into North America?Nature Physical Science, 1973
- Some Geophysical Observations on the Great Glen FaultNature, 1967