On the nomenclature of mode of failure transitions in rocks

Tectonophysics

Volumn 122, Issue 3-4, 1986, Pages 381-387

  Rutter, E H ^a  

^a IMPERIAL COLLEGE LONDON   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0022879364     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/0040-1951(86)90153-8     Document Type: Article

References (21)

1. The brittle—ductile transition in rocks
2. Foliated cataclasites
3. Stress and temperature in the bending lithosphere as constrained by experimental rock mechanics
4. The low temperature brittle—ductile transition in a quartzite and the occurrence of cataclastic flow in nature
5. Tectonics of slow spreading mid-ocean ridges and consequences of a variable depth to the brittle—ductile transition
6. Transition from brittle fracture to ductile flow in Solnhofen Limestone as a function of temperature, confining pressure and interstitial fluid pressure
7. Extensional Orogens
8. The Snake Range decollement; an exhumed mid-Tertiary brittle—ductile transition
9. Brittle to ductile transition due to large strains along the White Rock thrust, Wind River mountains, Wyoming
10. The generation of ductile and brittle shear bands in a low angle mylonite zone
11. The influence of interstitial water on the mechanical behaviour of calcite rocks
12. Experimental ‘syntectonic’ hydration of basalt
13. Fault zone models, heat flow and the depth distribution of earthquakes in the continental crust of the United States
14. Continental fault structure and the shallow earthquake source
15. Deformation of granitic rocks across the brittle—ductile transition
16. Intra-plate extensional tectonics of the eastern Basin-Range inferences on structural style from seismic reflection data regional tectonics and thermal-mechanical models of brittle—ductile deformation
17. Fracture as a mechanism of flow in naturally deformed, layered rocks
18. Mechanisms of crustal deformation
19. To stretch a continent
20. Controls of mylonitic compositional layering during non-cataclastic ductile deformation