Deformed anhydrite nodules: A new type of finite strain gauge in sedimentary rocks
- 1 April 1986
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 124 (3-4) , 309-323
- https://doi.org/10.1016/0040-1951(86)90207-6
Abstract
No abstract availableThis publication has 8 references indexed in Scilit:
- Preliminary estimates of the amount of continuous horizontal shortening across an Archean greenstone beltCanadian Journal of Earth Sciences, 1985
- Calculation of finite incremental deformations in ductile geological materials and structural modelsTectonophysics, 1983
- Natural indicators of solid-body rotation in deformed rocksTectonophysics, 1979
- Determination of stratigraphic thickness of strained unitsCanadian Journal of Earth Sciences, 1978
- Determination of geologic strain using randomly oriented strain markers of any shapeTectonophysics, 1977
- Distortion and dilatation in paleostrain analysisTectonophysics, 1977
- Sedimentological significance of nodular and laminated anhydriteGeology, 1975
- ON FOLDING DURING THREE-DIMENSIONAL PROGRESSIVE DEFORMATIONQuarterly Journal of the Geological Society, 1962