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A reappraisal of the Sibson-Scholz fault zone model: The nature of the frictional to viscous (‘brittle-ductile’) transition along a long-lived crustal-scale fault, Outer Hebrides, Scotland

Imber, J; Holdsworth, R.E; Butler, C.A; Strachan, R.A

A reappraisal of the Sibson-Scholz fault zone model: The nature of the frictional to viscous (‘brittle-ductile’) transition along a long-lived crustal-scale fault, Outer Hebrides, Scotland Thumbnail


Authors

J Imber

C.A Butler

R.A Strachan



Citation

Imber, J., Holdsworth, R., Butler, C., & Strachan, R. (2001). A reappraisal of the Sibson-Scholz fault zone model: The nature of the frictional to viscous (‘brittle-ductile’) transition along a long-lived crustal-scale fault, Outer Hebrides, Scotland. Tectonics, 20(5), 601-624. https://doi.org/10.1029/2000tc001250

Journal Article Type Article
Publication Date 2001-10
Deposit Date Oct 6, 2008
Publicly Available Date Mar 23, 2010
Journal Tectonics
Publisher European Geosciences Union
Peer Reviewed Peer Reviewed
Volume 20
Issue 5
Pages 601-624
DOI https://doi.org/10.1029/2000tc001250
Keywords Fractures, Faults, Role of fluids, Continental tectonics.
Publisher URL http://www.agu.org/journals/tc/tc0105/tc_20_5.html

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Copyright Statement
© 2001 American Geophysical Union. Imber, J., Holdsworth, R. E., Butler, C. A., Strachan, R. A., (2001), 'A reappraisal of the Sibson-Scholz fault zone model : the nature of the frictional to viscous ("brittle-ductile") transition along a long-lived, crustal-scale fault, Outer Hebrides, Scotland.', Tectonics., 20 (5). pp. 601-624.




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