When do dragfolds not develop into sheath folds in shear zones?
- 1 June 1999
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 21 (6) , 577-583
- https://doi.org/10.1016/s0191-8141(99)00065-6
Abstract
No abstract availableKeywords
This publication has 29 references indexed in Scilit:
- TranspressionPublished by Elsevier ,2003
- High-strain zones: a unified modelPublished by Elsevier ,1998
- Initiation of folding and boudinage in wrench shear and transpressionJournal of Structural Geology, 1994
- Transected folds and transpression: how are they associated?Journal of Structural Geology, 1992
- The origin of ridge-in-groove slickenside striae and associated steps in an S-C myloniteJournal of Structural Geology, 1992
- Progressive folding and foliation development in a sheared, coticule-bearing phylliteJournal of Structural Geology, 1991
- Tubular folds and sheath folds: definitions and conceptual models for their development, with examples from the Grapesvare area, northern SwedenJournal of Structural Geology, 1989
- A newly recognized type of slickenside striationJournal of Structural Geology, 1987
- Folds and the strain ellipsoid: a general modelJournal of Structural Geology, 1981
- Structural analysis of sheath folds with horizontal X-axes, northeast CanadaJournal of Structural Geology, 1981