Late Mesozoic strike slip movement on the Border Ranges Fault System in the Eastern Chugach Mountains, southern Alaska
- 10 April 1989
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 94 (B4) , 4321-4332
- https://doi.org/10.1029/jb094ib04p04321
Abstract
No abstract availableKeywords
This publication has 36 references indexed in Scilit:
- The development of fold axes oblique to the regional trendPublished by Elsevier ,2003
- Progressive development of structures in a ductile shear zonePublished by Elsevier ,2003
- Fabric development in shear zones: theoretical controls and observed phenomenaPublished by Elsevier ,2003
- The Himalayan Main Central Thrust pile and its quartz-rich tectonites in central NepalPublished by Elsevier ,2003
- Bulk kinematics from shear zone patterns: some field examplesJournal of Structural Geology, 1987
- Microstructural and fabric heterogeneities in fault rocks associated with a fundamental faultPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1986
- Bending anisotropy: A mechanical constraint on the orientation of fold axes in an anisotropic mediumTectonophysics, 1981
- The effect of the basal-prism mechanism switch on fabric development during plastic deformation of quartziteJournal of Structural Geology, 1981
- Axial directions of folds in rocks with linear/planar fabricsJournal of Structural Geology, 1981
- Development of sheath folds in shear regimesJournal of Structural Geology, 1980