Pseudotachylyte and the development of ultramylonite bands in the Saint-Barthélemy Massif, French Pyrenees

Journal of Structural Geology

Volumn 4, Issue 1, 1982, Pages 69-79

  Passchier, C W ^a  

^a Geologisch Instituut ^*  (Netherlands)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0019998938     PISSN: 01918141     EISSN: None     Source Type: Journal    
DOI: 10.1016/0191-8141(82)90008-6     Document Type: Article

References (22)

1. Mechanism of frictional fusion in fault zones
2. Microstructure of mylonites and their descriptive terminology
3. SP-Mylonites: Origin of some mylonites by superplastic flow
4. Superplasticity
5. An occurrence of Archean pseudotachylite from southeastern Manitoba
6. The pseudotachylyte problem
7. The Outer Hebrides Thrust
8. The relationship between Precambrian shear belts and modern fault systems
9. Microstructural and chemical transformations accompanying deformation of granite in a shear zone at Miéville, Switzerland; with implications for stress corrosion cracking and superplastic flow
10. Untersuchung der Aufschmelzung und Deformation der Pseudotachylite der Silvretta (Österreich, Schweiz)
11. Deformation and fusion of two fault rocks in relation to their depth of formation: the hyalomylonite of Langtang (Himalaya) and the pseudotachylytes of the Silvretta nappe (Eastern Alps)
12. The pseudotachylyte of the Gairloch District Rossshire Scotland
13. The transformation of pseudotachylyte to ultramylonite in a mylonite zone (abstract)
14. Superplastic flow in finegrained limestone
15. Generation of pseudotachylyte by ancient seismic faulting
16. Fault rocks and fault mechanisms
17. Transient discontinuities in ductile shear zones
18. Fault rocks as indicators of progressive shear deformation in the Guingamp region, Brittany
19. On mylonites in ductile shear zones
20. La géologie du massif du Saint-Barthélémy, Pyrenées, France
21. The geology of the central Pyrenees