|Slab detachment beneath eastern Anatolia: A possible cause for the formation of the North Anatolian fault|
C Faccenna, O Bellier, J Martinod, C Piromallo, V Regard
Earth and Planetary Science Letters 242 (1-2), 85-97, 2006
|Cumulative right-lateral fault slip rate across the Zagros—Makran transfer zone: role of the Minab—Zendan fault system in accommodating Arabia—Eurasia convergence in …|
V Regard, O Bellier, JC Thomas, D Bourlès, S Bonnet, MR Abbassi, ...
Geophysical Journal International 162 (1), 177-203, 2005
|Accommodation of Arabia‐Eurasia convergence in the Zagros‐Makran transfer zone, SE Iran: A transition between collision and subduction through a young deforming system|
V Regard, O Bellier, JC Thomas, MR Abbassi, J Mercier, E Shabanian, ...
Tectonics 23 (4), 2004
|Recent state of stress change in the Walker Lane zone, western Basin and Range province, United States|
O Bellier, ML Zoback
Tectonics 14 (3), 564-593, 1995
|Relationship between tectonism and volcanism along the Great Sumatran fault zone deduced by SPOT image analyses|
O Bellier, M Sébrier
Tectonophysics 233 (3-4), 215-231, 1994
|Late Cenozoic partitioning of oblique plate convergence in the Zagros fold‐and‐thrust belt (Iran)|
C Authemayou, D Chardon, O Bellier, Z Malekzadeh, E Shabanian, ...
Tectonics 25 (3), 2006
|Changes in the tectonic regime above a subduction zone of Andean type: The Andes of Peru and Bolivia during the Pliocene‐Pleistocene|
JL Mercier, M Sebrier, A Lavenu, J Cabrera, O Bellier, JF Dumont, ...
Journal of Geophysical Research: Solid Earth 97 (B8), 11945-11982, 1992
|Topography of the Calabria subduction zone (southern Italy): Clues for the origin of Mt. Etna|
C Faccenna, P Molin, B Orecchio, V Olivetti, O Bellier, F Funiciello, ...
Tectonics 30 (1), 2011
|Local erosion rates versus active tectonics: cosmic ray exposure modelling in Provence (south-east France)|
L Siame, O Bellier, R Braucher, M Sébrier, M Cushing, D Bourlès, ...
Earth and Planetary Science Letters 220 (3-4), 345-364, 2004
|Active deformation in Zagros—Makran transition zone inferred from GPS measurements|
R Bayer, J Chery, M Tatar, P Vernant, M Abbassi, F Masson, ...
Geophysical Journal International 165 (1), 373-381, 2006
|Cosmogenic dating ranging from 20 to 700 ka of a series of alluvial fan surfaces affected by the El Tigre fault, Argentina|
LL Siame, DL Bourlès, M Sébrier, O Bellier, J Carlos Castano, M Araujo, ...
Geology 25 (11), 975-978, 1997
|Analyses of the stress field in southeastern France from earthquake focal mechanisms|
E Baroux, N Béthoux, O Bellier
Geophysical Journal International 145 (2), 336-348, 2001
|Is the slip rate variation on the Great Sumatran Fault accommodated by fore‐arc stretching?|
O Bellier, M Sebrier
Geophysical Research Letters 22 (15), 1969-1972, 1995
|Recent tectonic reorganization of the Nubia-Eurasia convergent boundary heading for the closure of the western Mediterranean|
A Billi, C Faccenna, O Bellier, L Minelli, G Neri, C Piromallo, D Presti, ...
Bulletin de la Société Géologique de France 182 (4), 279-303, 2011
|Recent temporal change in the stress state and modern stress field along the North Anatolian Fault Zone (Turkey)|
O Bellier, S Över, A Poisson, J Andrieux
Geophysical Journal International 131 (1), 61-86, 1997
|Subsurface electrical imaging of anisotropic formations affected by a slow active reverse fault, Provence, France|
F Nguyen, S Garambois, D Chardon, D Hermitte, O Bellier, D Jongmans
Journal of applied geophysics 62 (4), 338-353, 2007
|From subduction to collision: Control of deep processes on the evolution of convergent plate boundary|
V Regard, C Faccenna, J Martinod, O Bellier, JC Thomas
Journal of Geophysical Research: Solid Earth 108 (B4), 2003
|Deformation partitioning in flat subduction setting: Case of the Andean foreland of western Argentina (28 S–33 S)|
LL Siame, O Bellier, M Sébrier, M Araujo
Tectonics 24 (5), 2005
|Plio-quaternary stress states in NE Iran: Kopeh Dagh and Allah Dagh-Binalud mountain ranges|
E Shabanian, O Bellier, MR Abbassi, L Siame, Y Farbod
Tectonophysics 480 (1-4), 280-304, 2010
|Quaternary slip rates along the northeastern boundary of the Arabia-Eurasia collision zone (Kopeh Dagh Mountains, Northeast Iran)|
E Shabanian, L Siame, O Bellier, L Benedetti, MR Abbassi
Geophysical Journal International 178 (2), 1055-1077, 2009