Constraints on deformation conditions and the origin of oceanic detachments: The Mid‐Atlantic Ridge core complex at 15°45′N
- 7 August 2003
- journal article
- Published by American Geophysical Union (AGU) in Geochemistry, Geophysics, Geosystems
- Vol. 4 (8)
- https://doi.org/10.1029/2002gc000472
Abstract
No abstract availableKeywords
This publication has 64 references indexed in Scilit:
- Submersible study of an oceanic megamullion in the central North AtlanticJournal of Geophysical Research, 2001
- Modeling heterogeneous stretching during episodic or steady rifting of the continental lithosphereGeology, 2001
- Ultramafic and gabbroic exposures at the Mid-Atlantic Ridge: geological mapping in the 15°N regionTectonophysics, 1997
- Evolution of rift basins and low-angle detachments in multilayer analog modelsGeology, 1997
- Abyssal peridotite mylonites: implications for grain-size sensitive flow and strain localization in the oceanic lithosphereTectonophysics, 1996
- Does magmatism influence low-angle normal faulting?Geology, 1993
- Emplacement of deep crustal and mantle rocks on the west median valley wall of the MARK area (MAR, 23°N)Tectonophysics, 1991
- Normal faulting in the upper continental crust: observations from regions of active extensionJournal of Structural Geology, 1989
- Mid-crustal Cretaceous roots of Cordilleran metamorphic core complexesGeology, 1988
- Role of tectonic denudation in warping and uplift of low-angle normal faultsGeology, 1984