Acknowledgements. This work was financed through the research project CGL2004-03657, funded by the Spanish Ministry of Education and Science. We thank J. Carreras, E. Druguet and L. M. Castaño for discussions on some aspects related to this work. We gratefully acknowledge G. Zulauf and T. Duretz, whose constructive reviews greatly improved the manuscript, and the editorial guidance of N. MancktelowPeer reviewedPublisher PD
M. Jean-Pierre Petit - Professeur, L.D.L., Montpellier Dir. ThèseM. Michel Barquins - Directeur de R...
Slates are metamorphic rocks characterized by the pervasive occurrence of cleavage or foliation prod...
Crustal scale fault zones extend below the brittle-ductile transition as ductile shear zones. Here w...
Fractures in rocks deformed under dominant ductile conditions typically form simultaneously with vis...
International audienceLocalized or distributed deformations in continental lithosphere are supposed ...
Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of Am...
The Earth\u2019s crust is generally considered to consist of distinct brittle and viscous (or \u201c...
International audienceThe mechanical coupling between brittle and ductile layers in the continental ...
Abstract: Field observation shows that brittle fracturing and ductile flow are often intimately rela...
Analogue models have been used to investigate the influence of planar mechanical anisotropy on the o...
Thèse publiée dans la collection des Mémoires de Géosciences Rennes (ISSN 1240-1498) : Mémoire n° 11...
AbstractWithin a low-grade ductile shear zone, we investigated exceptionally well exposed brittle fa...
The evolution of less ductile layers embedded in a more ductile matrix under simple progressive shea...
International audienceThe inherited localization model for shear zone development suggests that duct...
The variation of rock strength and stiffness, known as mechanical anisotropy, is expected at differe...
M. Jean-Pierre Petit - Professeur, L.D.L., Montpellier Dir. ThèseM. Michel Barquins - Directeur de R...
Slates are metamorphic rocks characterized by the pervasive occurrence of cleavage or foliation prod...
Crustal scale fault zones extend below the brittle-ductile transition as ductile shear zones. Here w...
Fractures in rocks deformed under dominant ductile conditions typically form simultaneously with vis...
International audienceLocalized or distributed deformations in continental lithosphere are supposed ...
Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of Am...
The Earth\u2019s crust is generally considered to consist of distinct brittle and viscous (or \u201c...
International audienceThe mechanical coupling between brittle and ductile layers in the continental ...
Abstract: Field observation shows that brittle fracturing and ductile flow are often intimately rela...
Analogue models have been used to investigate the influence of planar mechanical anisotropy on the o...
Thèse publiée dans la collection des Mémoires de Géosciences Rennes (ISSN 1240-1498) : Mémoire n° 11...
AbstractWithin a low-grade ductile shear zone, we investigated exceptionally well exposed brittle fa...
The evolution of less ductile layers embedded in a more ductile matrix under simple progressive shea...
International audienceThe inherited localization model for shear zone development suggests that duct...
The variation of rock strength and stiffness, known as mechanical anisotropy, is expected at differe...
M. Jean-Pierre Petit - Professeur, L.D.L., Montpellier Dir. ThèseM. Michel Barquins - Directeur de R...
Slates are metamorphic rocks characterized by the pervasive occurrence of cleavage or foliation prod...
Crustal scale fault zones extend below the brittle-ductile transition as ductile shear zones. Here w...