Erosion and rheology controls on synrift and postrift evolution: Verifying old and new ideas using a fully coupled numerical model
- 10 August 2001
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 106 (B8) , 16461-16481
- https://doi.org/10.1029/2001jb000433
Abstract
No abstract availableKeywords
This publication has 54 references indexed in Scilit:
- Dynamic link between the level of ductile crustal flow and style of normal faulting of brittle crustTectonophysics, 2000
- Abyssal hills formed by stretching oceanic lithosphereNature, 1998
- Erosion as a driving mechanism of intracontinental mountain growthJournal of Geophysical Research: Solid Earth, 1996
- Relative importance of strain rate and rheology for the mode of continental extensionGeophysical Journal International, 1995
- Erosional control of active compressional orogensPublished by Springer Nature ,1992
- Modes of continental lithospheric extensionJournal of Geophysical Research, 1991
- Variations in effective elastic thickness of the North American lithosphereNature, 1990
- A physical explanation of the relation between flank uplifts and the breakup unconformity at rifted continental marginsGeology, 1989
- Small-scale convection induced by passive rifting: the cause for uplift of rift shouldersEarth and Planetary Science Letters, 1986
- Limits on lithospheric stress imposed by laboratory experimentsJournal of Geophysical Research, 1980