Deformed anhydrite nodules: A new type of finite strain gauge in sedimentary rocks

Tectonophysics

Volumn 124, Issue 3-4, 1986, Pages 309-323

  Van Berkel, J T ^a   Torrance, J G ^a   Schwerdtner, W M ^a  

^a UNIVERSITY OF TORONTO   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0022872670     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/0040-1951(86)90207-6     Document Type: Article

References (22)

1. Evolution of Sverdrup Basin
2. Sedimentological significance of nodular and laminated anhydrite
3. On folding during three-dimensional progressive deformation
4. Piercement structures in the Arctic Islands
5. Origin and diagenesis of gypsum and anhydrite
6. Stratigraphy and sedimentation of the Otto Fiord Formation
7. Genesis of primary structures in anhydrite
8. Determination of geological strain using randomly oriented strain markers of any shape
9. Distortion and Dilatation in paleostrain analysis
10. Determination of stratigraphie thickness of strained units
11. Natural indicators of solid-body rotation in deformed rocks
12. Preliminary estimates of the amount of continuous horizontal shortening across an Archean greenstone belt
13. Calculation of finite incremental deformations in ductile geological materials and structural models
14. Carboniferous and Permian stratigraphy on Axel Heiberg Island and western Ellesmere Island, Canadian Arctic Archipelago
15. Geology of the Arctic Archipelago
16. Study of anticlines, faults and diapirs in the central Eureka Sound Fold Belt, Canadian Arctic Islands: Preliminary results
17. Origin of wall-and-basin structures—An intriguing tectonic-halokinetic feature on west-central Axel Heiberg island, Sverdrup Basin, Canadian Arctic Archipelago
18. Homogeneous deformation of the gneisses of Versterland, south-west Greenland