Stress based tectonic mechanisms at passive continental margins
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Publisher
American Geophysical Union
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1029/GD006p0147/fullpdf
Reference30 articles.
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2. Stresses in the lithosphere caused by crustal thickness inhomogeneities;Artyushkov;J. Geophys. Res.,1973
3. Evolution of young continental margins and formation of shelf basins;Bott;Tectonophysics,1971
4. Subsidence of Rockall Plateau and of the continental shelf;Bott;Geophys. J. Roy. Astron. Soc.,1972
5. Shelf subsidence in relation to the evolution of young continental margins;Bott,1973
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1. Buoyancy tectonic models of uplift and subsidence along high-angle faults in extensional and compressional tectonic regimes;Tectonophysics;1995-06
2. A high-strain rift model for the southern Gulf of Suez (Egypt);Geological Society, London, Special Publications;1995
3. An active thermoelastic rift mechanism;Journal of Geophysical Research: Solid Earth;1989-10-10
4. Influences of stress and temperature regimes on graben subsidence—a note;Tectonophysics;1987-02
5. Lithospheric stress and deformation;Reviews of Geophysics;1987
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