Constraints on geological strain rates: Arguments from finite strain states of naturally deformed rocks
- 10 January 1982
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 87 (B1), 311-321
- https://doi.org/10.1029/jb087ib01p00311
Abstract
No abstract availableKeywords
This publication has 26 references indexed in Scilit:
- Strain analysis of a shear zone in a granodioriteTectonophysics, 1978
- Fossil distortion and décollement tectonics of the Appalachian PlateauGeology, 1977
- Particle paths, displacement and progressive strain applicable to rocksTectonophysics, 1975
- Finite strain estimates from the dalradian dolomitic formation, Islay, Argyll, ScotlandTectonophysics, 1973
- The geometric effects of volume change during deformation processesTectonophysics, 1973
- Determination of strain ellipses from deformed ammonoidsTectonophysics, 1973
- Strain analysis of deformed Pipe Rock in the Moine Thrust zone, northwest ScotlandTectonophysics, 1971
- Non-random sedimentary fabrics and their modification by strainTectonophysics, 1971
- A technique of finite strain analysis using elliptical particlesTectonophysics, 1969
- Pebble elongation parallel to the axis of rollingTschermaks Mineralogische und Petrographische Mitteilungen, 1966