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Ventoux-Lure Massif

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Journal Article
Published: 01 March 1992
Bulletin de la Société Géologique de France (1992) 163 (2): 147–158.
Journal Article
Published: 01 September 1988
Bulletin de la Société Géologique de France (1988) IV (5): 733–737.
... tectonics rifting sea-floor spreading sedimentary basins sedimentation Southern Europe subsidence tectonics tectonophysics Tethys unconformities Upper Jurassic Var France Ventoux-Lure Massif Vocontian Basin Western Alps Western Europe ...
Journal Article
Published: 01 November 2010
Bulletin de la Société Géologique de France (2010) 181 (6): 503–530.
... the Ventoux-Lure thrust zone in Provence during the Miocene. Southward, this gravity sliding vanishes approaching the E-W trending structural high of the Eocene Pyrénéo-Provençal orogenic belt in southern Provence. Located between the Mediterranean Sea to the south, the Hercynian basement of the Massif...
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Journal Article
Published: 01 November 2010
Bulletin de la Société Géologique de France (2010) 181 (6): 477–501.
... been used to document for the first time in considerable detail the existence of a 140 by 200 km large and 12 km thick Mesozoic basin between the Durance fault to the east and the Cévennes fault to the west. This basin extends to the north of the Lure-Ventoux mountain below the Diois-Baronnies area...
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Journal Article
Published: 01 July 2013
Bulletin de la Société Géologique de France (2013) 184 (4-5): 501–514.
.... Montenat C. Ott d’Estevou P. ( 1992 ). – Evènements tectoniques crétacés dans la partie méridionale du bassin subalpin (massif Ventoux-Lure et partie orientale de l’arc de Castellane, SE France). Implications géodynamiques . – Bull. Soc. géol. Fr. , 163, 2 , 147 – 158 . Homberg C. Hu...
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Journal Article
Published: 01 November 2010
Bulletin de la Société Géologique de France (2010) 181 (6): 476.
... in recent time by radial collapse of the Alps. The incipient stage of this gravity sliding occurred during the Late Oligocene in the Diois-Baronnies (the former Mesozoic Vocontian basin), and then rapidly progressed to the south across the Ventoux-Lure thrust zone in Provence during the Miocene. Guillou...
Journal Article
Published: 01 March 2011
Bulletin de la Société Géologique de France (2011) 182 (2): 95–110.
..., La Fare). North-verging structures exist to the east of the MDF (e.g. Sainte Baume, Sainte Victoire) and to the west of the SCF (e.g. Istres, Anelier thrusts). This indicates that these two faults are major transfer faults [e.g., Molliex, 2009 ]. The Mont Ventoux-Montagne de Lure ridge...
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Image
Figure 2. (A) Kinematic data of Eocene to early Miocene age describing the principal Western Alpine arc. Arrows represent particle-displacement paths derived principally from linear indicators of relative motion, such as stretching lineations in mylonites and wear grooves and crystal fibers on fault planes. Arrows show sense of shear. The location of data is indicated by a filled circle. Data are principally taken from Platt et al. (1989a). New data in southeast France are from Fry (1989a, 1989c), Butler (1992a), Meckel et al. (1996), Bürgisser and Ford (1998), and Lickorish and Ford (1998). The Pelvoux–southern Belledonne massifs are shaded gray as they formed a paleogeographic high. Internally derived exotic flysch nappes were emplaced onto the foreland. First the Embrunais-Ubaye nappes were emplaced toward the southwest (Kerckhove, 1969; Merle and Brun, 1984), and later the Prealps were emplaced toward the northwest (Mosar et al., 1996). Abbreviations are mainly the same as in Figure 1. FPF—Frontal Pennine fault, NSC—northern Subalpine chains. (B) Middle Miocene to Holocene kinematic data. The late Miocene–Pliocene data occur in the Jura arc (shaded area) and the Vercors and Chartreuse massifs. These smoothed and interpolated strain trajectories are derived principally from fault-slip data and stylolite peaks (Philippe et al., 1996). Arrows indicate sense of shear. Jura fold axial traces are shown by dashed lines. White areas within the shaded Jura indicate synclines filled with Tertiary sedimentary rocks. In southeast France, middle to late Miocene and Pliocene data represent principal shortening axes and sense of shear derived mainly from fault-slip data. Middle to late Miocene data were taken from Fry (1989a, 1989c), Platt et al. (1989a), Ford and Stahel (1995), Ritz (1991), Lickorish and Ford (1998). Pliocene data were from Ritz (1991) and Champion et al. (2000), whereas Quaternary data were from Ritz (1991). Abbreviations are the same as in Figure 1 except CA—Castellane arc, V-L—Ventoux-Lure fault, Dur.—Durence fault, Lub.—Luberon fault. External crystalline massifs were exhumed at this time around the arc
Published: 01 September 2002
and Stahel (1995) , Ritz (1991) , Lickorish and Ford (1998) . Pliocene data were from Ritz (1991) and Champion et al. (2000) , whereas Quaternary data were from Ritz (1991) . Abbreviations are the same as in Figure 1 except CA—Castellane arc, V-L—Ventoux-Lure fault, Dur.—Durence fault, Lub.—Luberon
Journal Article
Published: 01 December 1997
Russ. Geol. Geophys. (1997) 38 (12): 2000–2011.
... of Baronnies, where central massifs of the Lure anticline or monoclinal ridges of the northern limb of the anticlinal Ventoux Massif regenerate. When folded mountains form, the upper layered tectonic plate reduces (is heaped) at the cost of transportation of rock volumes to the upper free half-space...
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Journal Article
Published: 01 December 2004
Bulletin of the Seismological Society of America (2004) 94 (6): 2137–2163.
...-Alpilles 5.5 785 5 Ventoux-Lure 5.5 685 5 psha easily enables the consideration of a hypothesis based on the input assumptions of the seismicity model, such as the size and the recurrence of maximum magnitude of each source. We studied the possibility of integrating the occurrence...
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Journal Article
Journal: GSA Bulletin
Published: 01 September 2002
GSA Bulletin (2002) 114 (9): 1089–1107.
... and Stahel (1995) , Ritz (1991) , Lickorish and Ford (1998) . Pliocene data were from Ritz (1991) and Champion et al. (2000) , whereas Quaternary data were from Ritz (1991) . Abbreviations are the same as in Figure 1 except CA—Castellane arc, V-L—Ventoux-Lure fault, Dur.—Durence fault, Lub.—Luberon...
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Journal Article
Published: 01 January 2010
Bulletin de la Société Géologique de France (2010) 181 (1): 3–18.
... calcareous nannofossils and stable isotopes .” Tübinger Mikropaléontologische Mitteilungen , 27 . Hibsch C. , Kandel D. , Montenat C. & Ott D’Estevou P. ( 1992 ). “ Evénements tectoniques crétacés dans la partie méridionale du bas-sin subalpin (massif Ventoux-Lure et...
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Journal Article
Published: 24 September 2024
Bulletin de la Société Géologique de France (2025) 195 (1): 17.
...: Cevennes fault, NF: Nîmes fault, MDF: Moyenne Durance fault, NCFS: Northeast Cévennes Fault System, VF: Valence fault, VT: Vercors thrust, LT: Lance thrust, VLT: Ventoux-Lure thrust, LuT: Luberon thrust, DN: Digne nappe, S.S: Saou syncline, S.A: Saou anticline, D.S: Dieulet syncline, P.A: Puygiron...
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Journal Article
Published: 01 July 2015
Bulletin de la Société Géologique de France (2015) 186 (4-5): 223–241.
... . – Thèse Sci. , Aix-Marseille Université, Centre Saint-Charles , Marseille , 252 p. Hibsch C. Kandel D. Montenat C. Ott D’estevou P. ( 1992 ). – Evénements tectoniques crétacés dans la partie méridionale du bassin subalpin (massif Ventoux-Lure et partie occidentale de l’Arc de...
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Journal Article
Published: 01 November 2008
Bulletin de la Société Géologique de France (2008) 179 (6): 551–568.
... crétacés dans la partie méridionale du bassin subalpin (massif Ventoux-Lure et partie orientale de l’arc de Castellane, SE France); implications géodynamiques. l’Eocène .” Bull. Soc. géol. Fr ., ( 2 ), 163 , 147 – 158 Hippolyte J.C. & Dumont T. ( 2000 ). “ Identification...
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Journal Article
Published: 03 October 2024
Journal of the Geological Society (2024) 181 (6): jgs2024-042.
... and thus less influence from the Durance fault. This may be due to the important compartmentation of the region. The Sorine diapir and the St-Geniez series are located at the intersection of two inherited basement faults, the east–west-trending VentouxLure fault and the NE–SWW-trending Durance fault (e.g...
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Journal Article
Published: 01 March 2009
Bulletin de la Société Géologique de France (2009) 180 (2): 105–115.
... C. ( 1980 ). “ La Provence . Introduction à la géologie du sud-est. In: 26 e CGI, Paris . Hibsh C. , Kandel D. , Montenat C. & Ott D’estevou P. ( 1992 ). “ Evénements tectoniques crétacés dans la partie méridionale du bassin subalpin (massif de Ventoux-Lure...
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Journal Article
Published: 01 November 2010
Bulletin de la Société Géologique de France (2010) 181 (6): 565–581.
... ). – The geometry of a deformed carbonate slope-basin transition: The Ventoux-Lure fault zone, SE France . – Tectonics , 14 , 1393 – 1410 . Fournier M. , Agard Ph. & Petit C. ( 2008 ). – Micro-tectonic constraints on the evolution of the Barles half-window (Digne nappe, southern Alps...
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Journal Article
Published: 07 October 2024
Bulletin de la Société Géologique de France (2025) 195 (1): 19.
... ; Manchuel et al. , 2018 ; Bollinger et al. , 2021 ). In addition, the region shows ancient surface ruptures (paleoseismic) identified on the Nîmes Fault, the Ventoux Lure thrust and the La Rouvière Fault ( Ritz et al. , 2021 , Bellier et al. , 2021 ), evidence for its past and probably significant...
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Journal Article
Published: 26 October 2023
Bulletin de la Société Géologique de France (2023) 194 (1): 13.
... to the termination of the continental shelf ( i.e. pre-Vocontian settings sensu Frau et al. , 2018 ) and is mostly characterised by fine-grained calcisiltite facies ( Tabs. 2 and 4 ). The Vocontian Basin sensu stricto is located further seaward and delineated by major faulting systems ( e.g. VentouxLure...
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