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Grande Anse Formation

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Journal Article
Published: 06 August 2020
Canadian Journal of Earth Sciences (2021) 58 (3): 209–224.
... equivalent, but mostly unstudied, ∼600 m thick succession of Grande Anse Formation lies in angular unconformity on folded and faulted Boss Point and basal Little River formations. Grande Anse Formation sedimentology indicates four lithofacies associations: floodplain (LA1), braided channel (LA2), sheet flood...
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Sedimentary logs and paleoflow data for the <span class="search-highlight">Grande</span> <span class="search-highlight">Anse</span> <span class="search-highlight">Formation</span>, includin...
Published: 06 August 2020
Fig. 4. Sedimentary logs and paleoflow data for the Grande Anse Formation, including east and west Maringouin Peninsula locations and Minudie Point location (locations map is modified from Craggs et al. 2017 ). [Colour online.]
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Identified lithofacies of <span class="search-highlight">Grande</span> <span class="search-highlight">Anse</span> <span class="search-highlight">Formation</span>, modified from  Miall (1978...
Published: 06 August 2020
Table 1. Identified lithofacies of Grande Anse Formation, modified from Miall (1978 , 2006 ).
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Identified lithofacies associations of the <span class="search-highlight">Grande</span> <span class="search-highlight">Anse</span> <span class="search-highlight">Formation</span>, modified ...
Published: 06 August 2020
Table 2. Identified lithofacies associations of the Grande Anse Formation, modified from Miall (2006) . Note: Please refer to Table 1 for lithofacies code definitions.
Journal Article
Published: 23 September 2021
Journal of Sedimentary Research (2021) 91 (9): 969–985.
... Heritage Site, the post–Boss Point Formation succession comprises an ∼ 3 km succession of strata assigned to the Little River, Joggins, Springhill Mines, and Ragged Reef formations. North of the Minudie anticline, the Grande Anse Formation lies in angular unconformity on the Boss Point and basal Little...
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Photomicrographs (XPL) showing samples dominated by carbonate cements and r...
Published: 23 September 2021
Fig. 7.— Photomicrographs (XPL) showing samples dominated by carbonate cements and rock fragments A) J-2, Joggins Formation, B) G3-3 Grande Anse Formation, C) S2-8 Grande Anse Formation, note reworked fossil with oxide rim, blue arrow. D) A non-carbonate-cemented Grande Anse sandstone (S1
Journal Article
Published: 01 December 2007
Journal of the Geological Society (2007) 164 (6): 1113–1118.
...Howard J. Falcon-Lang; Michael J. Benton; Matthew Stimson Abstract Trackways representing the earliest evidence for the origin of reptiles (amniotes) are reported from the basal Pennsylvanian Grande Anse Formation, New Brunswick, Canada. Amniote characters include pentadactyl manus and pes, slender...
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Conceptual model of the evolution of the western Cumberland Basin. (A) Vise...
Published: 06 August 2020
, early Langsettian, Little River Formation deposition started in the south side of salt wall and increases loading on evaporitic strata of the Windsor Group (E; option one), deposition of the Grande Anse Formation in the north side of the salt wall, at same time as the deposition of the Joggins
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Geological setting. ( a ) Location of trackway site at Shepody Bay, eastern...
Published: 01 December 2007
Fig. 1.  Geological setting. ( a ) Location of trackway site at Shepody Bay, eastern side of the Maringouin Peninsula, New Brunswick (45°47′48″N, 64°300′29″W), within the Grand Anse Formation (after Davies et al . 2005 ); ( b ) Lower Pennsylvanian stratigraphy of the Cumberland Basin
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Conceptual model of the evolution of the western Cumberland Basin during Ca...
Published: 23 September 2021
increases loading on evaporitic strata of the Windsor Gp. 3A) Option one: deposition of the Grande Anse Formation commences on the north side of the salt wall, in a rejuvenated Black Point sub-basin, at same time as the deposition of the Joggins, Springhill Mines, and Polly Brook formations in the Athol
Journal Article
Published: 01 September 2008
Journal of the Geological Society (2008) 165 (5): 983–987.
...-Lang et al . (2007 , p. 1113) claim ‘trackways representing the earliest evidence for the origin of reptiles (amniotes) are reported from the basal Pennsylvanian Grande Anse Formation, New Brunswick’. We note inaccuracies in the paper and bring attention to various lines of evidence, any one of which...
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Correlation model (second option,  Figs. 5A – 6B ): (A) Lower part of the G...
Published: 06 August 2020
Fig. 12. Correlation model (second option, Figs. 5A – 6B ): (A) Lower part of the Grande Anse and Ragged Reef formations that are separated by a salt well (B). Upper part of the Grande Anse and Ragged Reef formations. [Colour online.]
Journal Article
Published: 01 March 2003
Bulletin de la Société Géologique de France (2003) 174 (2): 125–140.
... sources, as their products are rarely hydrothermalized and are more vesicular. The breccia formation, and especially the progressive breaking up occurring during the debris avalanche displacement, indicates the existence of high speed transport. In the Cap La Houssaye coastal area, abrasion and striation...
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1972
AAPG Bulletin (1972) 56 (1): 114–127.
... and formal stratigraphic names proposed. The Anse la Roche Formation of coarse volcaniclastics, limestone, and subordinate silts contains a Pliolepidina tobleri foraminiferal fauna associated with late Eocene plankton. Early Oligocene rocks were not recorded. Late Oligocene to early Miocene volcaniclastics...
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Journal Article
Published: 16 March 2005
Canadian Journal of Earth Sciences (2005) 42 (3): 259–272.
...Hugues Longuépée; Pierre A. Cousineau Abstract The Cambrian Anse Maranda Formation is a glauconite-bearing clastic succession within the Quebec Reentrant. It is part of the Appalachians Humber Zone, particularly of the shale – feldspathic sandstone assemblage, which represents the rift-to-drift...
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Journal Article
Published: 01 December 1988
Bulletin of Canadian Petroleum Geology (1988) 36 (4): 379–387.
... and species variation within the West Point Formation. The majority of coral colonies found in the West Point Reef Complex are con- sidered to have been preserved in their life growth position, although those in a few facies (e.g. Cap de l'Enfer, Pointe Pillar and proximal Anse Beebe facies) show evidence...
Journal Article
Published: 01 June 2001
Bulletin of Canadian Petroleum Geology (2001) 49 (2): 217–237.
..., the depositional facies oscillated between shoreline sands (Anse Cascon Formation) and peritidal limestones fringed by coralgal knob reefs and shallow subtidal lime sands (La Vieille Formation) ( Bourque et al., 1986 ; Desrochers and Bourque, 1989 ; Lavoie et al., 1992 ). One significant exception is a high...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1964
AAPG Bulletin (1964) 48 (4): 437–464.
.... Clarke (1900 , 1908 , 1913 ) grouped Logan’s members of the Siluro-Devonian Forillon Peninsula section in eastern Gaspé into three formations, the St. Alban, Cape Bon Ami, and Grande Greve. Schuchert and Dart (1926) mapped the Port Daniel area and proposed a subdivision for the thick Silurian section...
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Journal Article
Published: 24 February 2003
Canadian Journal of Earth Sciences (2003) 40 (2): 177–205.
... and Hubert 1995 b ). The lower part of the Anse-Maranda Formation at the base of the Bacchus Nappe is possibly also correlative ( Landing et al. 2002 ) (Fig.  7 ). Where exposed, the thickness of these rock units is rather fairly constant at roughly 600 meters. The lower part of this sandstone interval...
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Journal Article
Published: 01 December 1986
Bulletin of Canadian Petroleum Geology (1986) 34 (4): 452–489.
... the frame organisms. Growth Fig. 7. Stacking of individual bioherms of biostromal-biohermal lime- stone facies of La Vieille Formation above well-bedded calcarenite facies at right. Anse a la Barbe River section, Gascons, Chaleurs Bay. 458 P.-A. BOURQUE et al. cavities in both types of boundstone...