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Cannes-de-Roches Basin

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Journal Article
Journal: GSA Bulletin
Published: 01 December 2003
GSA Bulletin (2003) 115 (12): 1538-1551.
...Pierre Jutras; Gilbert Prichonnet; Steven McCutcheon Abstract Juxtaposition of the Mississippian Ristigouche and Cannes-de-Roches Basins, which are subbasins of the composite late Paleozoic Maritimes Basin, occurred through dextral movement along the northwest-striking Percé Fault system...
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Journal Article
Published: 29 November 2000
Canadian Journal of Earth Sciences (2000) 38 (1): 1-19.
... to Percé. From the above-mentioned paleocurrent patterns, we conclude that the much thinner Cannes-de-Roches Cove sequence, which has a distinct paleocurrent trend, was not deposited in the Ristigouche Basin, but in an adjacent one, as was first proposed by Alcock ( 1935 ), that we herein refer...
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Paleogeographic reconstruction of the Ristigouche, <b>Cannes</b>-<b>de</b>-<b>Roches</b>, and Ma...
Published: 29 November 2000
Fig. 16. Paleogeographic reconstruction of the Ristigouche, Cannes-de-Roches, and Maritimes basins during sedimentation of the Bonaventure Formation.
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Figure 13. (A) Paleogeography of the Bonaventure Formation in the <b>Cannes</b>-<b>de</b>...
Published: 01 December 2003
Figure 13. (A) Paleogeography of the Bonaventure Formation in the Cannes-de-Roches Basin ( Rust, 1981 ) and Ristigouche Basin ( Jutras et al., 2001 ). The thin Cannes-de-Roches succession of Bonaventure Formation beds (lower and middle members of the abandoned Cannes-de-Roches Formation
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Figure 4. Stratigraphic columns a to e and cross section A–B, showing the m...
Published: 01 December 2003
Figure 4. Stratigraphic columns a to e and cross section A–B, showing the main structures and stratigraphic units of the Percé area (legend, localities, and transect are shown in Fig. 3 ). A sketch of the open drag fold adjacent to the Cap Blanc Fault is shown in inset. C.-d.-R BasinCannes-de
Journal Article
Published: 19 July 2005
Canadian Journal of Earth Sciences (2005) 42 (5): 815-832.
... on the nearly completely digested host sediment of the La Coulée Calcrete in the Cannes-de-Roches Basin, but the presence of incompletely digested basalt gravels floating in the calcrete mass indicates that it was a compositionally different conglomerate than that of the La Coulée Formation in the Ristigouche...
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Journal Article
Journal: GSA Bulletin
Published: 01 September 2004
GSA Bulletin (2004) 116 (9-10): 1074-1086.
... Formation in both the Ristigouche and Cannes-de-Roches Basins ( Jutras et al., 1999 , 2001 ). Bearing at the base of its clastic succession a massive, ≤12-m-thick, groundwater calcrete hardpan, the La Coulée Formation is inferred to have been deposited in the vicinity of an evaporitic basin ( Jutras et al...
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Figure 8. (A) View from the southeast side of the 200-m-high Pic <b>de</b> l&#x27;Auror...
Published: 01 December 2003
Figure 8. (A) View from the southeast side of the 200-m-high Pic de l'Aurore. The thick, flat-lying succession of Bonaventure Formation beds within the Ristigouche Basin contrasts with that succession's thin and steeply dipping equivalent within the Cannes-de-Roches Cove succession
Journal Article
Published: 12 September 2018
Bulletin de la Société Géologique de France (2018) 189 (3): 12.
... for the Plan de la Tour granite, Moulin Blanc granite, and Bornes gneiss in the Maures massif; of about 93 Ma for the Saint Tropez granite; and around 140 Ma in the Tanneron massif west of Cannes ( Fig. 9 ; Lucazeau and Mailhé, 1986 ; Morillon, 1992 , 1997 ; Jakni, 2000 ). In the ZFT data...
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Journal Article
Journal: Palynology
Published: 01 November 2016
Palynology (2016) 40 (3): 379-409.
...Clinton Foster; Reed Wicander Abstract A well-preserved and moderately diverse organic-walled microphytoplankton assemblage was recovered from the subsurface Lower Ordovician Nambeet Formation, Canning Basin, Western Australia. The microphytoplankton assemblage consists of prasinophyte phycomata...
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Journal Article
Published: 01 September 2016
Canadian Journal of Earth Sciences (2016) 54 (1): 33-51.
... Jurassic distant river supply through the Fundy Basin is encouraging for deep-water reservoir quality in the western part. Les grès du Jurassique et du Crétacé dans le sous-bassin Shelburne et le bassin Fundy, au large de la Nouvelle-Écosse, sont peu connus mais ils sont actuellement d’intérêt...
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Tectonostratigraphic model for the Viséan of eastern Gaspésie. (A) Depositi...
Published: 19 July 2005
of the southern block of the Grande-Rivière fault (Ristigouche Basin) and the pull-apart reactivation of faults binding the Cannes-de-Roches Basin (modified from Jutras et al. 2001 ). Refer to Fig.  1 for legend.
Journal Article
Published: 01 February 1990
Journal of the Geological Society (1990) 147 (1): 41-57.
.... Published by the Geological Survey of Tanganyika. Scale 1:2,000,000. Gilboy, C. F. 1970. The geology of the Gariboro region of Southern Ethiopia. PhD thesis University of Leeds. Giraud P. Les roches basiques de la region d’Andriamena et leur mineralisation chromifere. Thése Cleremont...
Journal Article
Published: 01 January 2000
Canadian Journal of Earth Sciences (2000) 36 (10): 1671-1695.
... et de six roches vertes, appartenant aux trois lots structuraux du plateau Yukon–Tanana au centre-est de l’Alaska qui suivent: l’assemblage Lake George (LG) composé de gneiss oeillés, schiste à quartz–mica, quartzite, et amphibolite des périodes Dévono-Mississippien; l’assemblage de Taylor Mountain...
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Journal Article
Published: 01 May 2001
Geological Magazine (2001) 138 (3): 345-363.
... to initial opening of a Neotethyan ocean basin adjacent to a rifted continental margin. Radiolarites located stratigraphically higher in the coherent succession studied are dated as Middle Jurassic (Late Bathonian–Early Callovian). Similar-aged radiolarites are depositionally associated with ophiolitic rocks...
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Journal Article
Published: 01 June 2006
Canadian Journal of Earth Sciences (2006) 43 (5): 593-616.
... Lake Formation samples plotted on the Ti/100–Zr–Y*3 diagram of Pearce and Cann ( 1973 ). Most samples again plot within the WPB field. The two outliers represent fractionated intermediates. Other fields on diagram include volcanic-arc basalts (VAB) and MORB. Fig. 15. Strike–slip basin...
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Journal Article
Published: 01 May 2015
Canadian Journal of Earth Sciences (2015) 52 (7): 431-443.
... a lower intercept age of ∼201 Ma. Des roches mafiques et ultramafiques affleurent en amas de schistes à talc–antigorite–olivine (± orthopyroxène) et amphibole–chlorite, de taille décimétrique à centimétrique, interstratifiés dans le dans le schiste pélitique Kluane du sud-ouest du Yukon...
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Journal Article
Published: 24 April 2013
Canadian Journal of Earth Sciences (2013) 50 (8): 826-846.
... and fragmented by faults. Nous présentons les résultats d’une nouvelle cartographie, de géochimie sur la roche entière, des éléments majeurs, mineurs et traces, et de pétrographie de roches méta-ignées du secteur du mont Veta dans la partie la plus à l’ouest du terrane allochtone Yukon–Tanana (YTT) dans le...
Journal Article
Published: 25 December 2007
Canadian Journal of Earth Sciences (2007) 44 (9): 1267-1289.
... inférieure de Little Salmon comprend des roches surtout volcano-clastiques qui proviennent de l’érosion d’unités datant du Mississippien précoce et plus anciennes, incluant les roches de l’arc continental de Little Kalzas. Au-dessus d’un membre de calcaire médian, la succession supérieure de la Formation de...
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Journal Article
Published: 18 January 2018
Canadian Journal of Earth Sciences (2018) 55 (4): 356-372.
..., the Hopewell Cape Formation Shin Member (including the abandoned Bonaventure and Cannes-de-Roches formations) was sourced from steep fault scarps and deposited in proximal, gravelly alluvial fans and braidplains. Based on stratigraphic relationships ( Figs. 1 and 2 ), deposition of the fault-controlled...
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