Three‐dimensional gravity study of the Mid‐Atlantic Ridge: Evolution of the segmentation between 28° and 29°N during the last 10 m.y.
- 10 February 1994
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 99 (B2) , 3015-3029
- https://doi.org/10.1029/93jb02361
Abstract
No abstract availableKeywords
This publication has 13 references indexed in Scilit:
- Emplacement of deep crustal and mantle rocks on the west median valley wall of the MARK area (MAR, 23°N)Published by Elsevier ,2003
- Mid-Ocean Ridges: Discontinuities, Segments and Giant CracksScience, 1991
- Three‐dimensional analysis of gravity anomalies in the Mark Area, Mid‐Atlantlc Ridge 23°NJournal of Geophysical Research, 1991
- Evidence from gravity data for focusedmagmatic accretionalong the Mid-Atlantic RidgeNature, 1990
- Gravimetry on the Erimo Seamount, JapanTectonophysics, 1989
- Three‐dimensional flow and temperature perturbations due to a transform offset: Effects on oceanic crustal and upper mantle structureJournal of Geophysical Research, 1988
- Gravity anomalies of the ridge-transform system in the South Atlantic between 31 and 34.5 S: Upwelling centers and variations in crustal thicknessMarine Geophysical Research, 1988
- A least‐squares smooth fitting for irregularly spaced data: Finite‐element approach using the cubic B-spline basisGeophysics, 1986
- Techniques for interpretation of geoid anomaliesJournal of Geophysical Research, 1979
- An analysis of the variation of ocean floor bathymetry and heat flow with ageJournal of Geophysical Research, 1977