Effect of depleted continental lithosphere counterflow and inherited crustal weakness on rifting of the continental lithosphere: General results

Author:

Beaumont Christopher,Ings Steven J.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference51 articles.

1. Crustal structure: A key constraint on the mechanism of ultra-high-pressure rock exhumation;Beaumont;Earth Planet. Sci. Lett.,2009

2. Tectonic denudation of the upper mantle along passive margins: A model based on drilling results (ODP leg 103, western Galicia margin, Spain);Boillot;Tectonophysics,1987

3. Dynamical models of the role of crustal shear zones in symmetric continental extension;Braun;Earth Planet. Sci. Lett.,1989

4. Residual depth anomalies on the Iberian, Newfoundland, Labrador and Nova Scotian margins; implications for their lithosphere mass and density distribution;Cooper;Eos Trans. AGU,2007

5. Evidence for lateral variation in lithospheric mantle density across the ocean-continent transition of the Iberia and Newfoundland conjugate rifted margins;Cooper;Geophys. Res. Abstr.,2009

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