The morphology and tectonics of the Mark area from Sea Beam and Sea MARC I observations (Mid-Atlantic Ridge 23° N)
- 1 March 1988
- journal article
- Published by Springer Nature in Marine Geophysical Research
- Vol. 10 (1-2), 59-90
- https://doi.org/10.1007/bf02424661
Abstract
No abstract availableKeywords
This publication has 35 references indexed in Scilit:
- Morphology and crustal structure of the Kane Fracture Zone Transverse RidgeJournal of Geophysical Research, 1988
- Bathymetric artifacts in Sea Beam data: How to recognize them and what causes themJournal of Geophysical Research, 1986
- Chemical controls on ecology in a coastal wetlandEos, 1986
- Marine Multichannel Seismology WorkshopEos, 1984
- Anomalously thin crust in oceanic fracture zones: New seismic constraints from the Kane Fracture ZoneJournal of Geophysical Research, 1984
- A tectonic model for ridge-transform-ridge plate boundaries: Implications for the structure of oceanic lithosphereTectonophysics, 1984
- Compositional variation in normal MORB from 22°–25°N: Mid‐Atlantic Ridge and Kane Fracture ZoneJournal of Geophysical Research, 1981
- Volcanics and structure of the famous Narrowgate Rift: evidence for cyclic evolution: AMAR 1Journal of Geophysical Research, 1981
- Morphology and tectonics of the inner rift valley at lat 36°50′N on the Mid-Atlantic RidgeGSA Bulletin, 1977
- Crustal Plates in the Central Atlantic: Evidence for at Least Two Poles of RotationScience, 1969