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La Crete Subbasin

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Journal Article
Published: 01 December 1995
Bulletin of Canadian Petroleum Geology (1995) 43 (4): 433–460.
... platform to the La Crete Subbasin. In the La Crete Subbasin the potential hydrocarbon source rock is a metre-thick laminite (the bituminous marker) which was deposited in water depths of only 20-40 m. In contrast to the Duvernay Formation, high organic productivity (planktonic) was the first-order control...
Journal Article
Published: 01 December 1987
Bulletin of Canadian Petroleum Geology (1987) 35 (4): 416–429.
... of the La Crete subbasin. The exposed sequence embraces units A, B and C. Antiform structures and associated brecciation in these strata can be related to the formation of submarine pseudo-anticlines, tepee structures and localized collapse associated with the removal of evaporites of the underlying...
Journal Article
Published: 01 March 1997
Bulletin of Canadian Petroleum Geology (1997) 45 (1): 25–53.
..., suggest significant hydrocarbon potential in Deer Lake Subbasin. Likewise, Late Vis6an correlatives elsewhere in Atlantic Canada and adjacent offshore areas may also have significant, but currently unconfirmed, hydrocarbon potential. RI~SUM~ La formation Rocky Brook (groupe Deer Lake) est compos~e de...
Journal Article
Published: 01 September 1996
Bulletin of Canadian Petroleum Geology (1996) 44 (3): 508–529.
... drainait en direction nord-ouest sur le bouclier canadien. Le plus important bassin de drainage dans la partie centrale de l’avant-pays s’écoula vers le nord-ouest, puis tourna directement vers l’ouest, comme le firent deux autres bassins entre la crête de Pembina et la ceinture de charriage. Un bassin...
Journal Article
Journal: GSA Bulletin
Published: 01 July 2008
GSA Bulletin (2008) 120 (7-8): 976–993.
... seems largely confined to the period between ca. 5 and 3 Ma, why southward motion of Crete continues today, why there is no record of compression accompanying the uplift, and why the timing and rate of uplift vary from subbasin to subbasin. An alternative scenario with quantitative predictions...
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Journal Article
Published: 01 June 1987
Bulletin of Canadian Petroleum Geology (1987) 35 (2): 123–142.
... estuariens; 2)une sequence interstratifiee d'argiles foncees, de gres dont la granulometrie augmente vers le haut et de filons de charbon jusqu'~ 8 m d'epais- seur, deposes dans une plaine alluviale; 3) des gres bien classes, et de petites quantites d'argiles en partie calcaires, interprOtes comme cretes...
Journal Article
Published: 01 March 2016
Bulletin of Canadian Petroleum Geology (2016) 64 (1): 1–23.
... extérieure de la baie, les crêtes du socle rocheux sont recouvertes de boues et de moraines glaciomarines mélangées d’icebergs. En dessous de cette couverture, la réinterprétation des analyses palynologiques du puits A-36 ne reflète que le groupe de Codroy du Viséen. Une corrélation pourrait exister entre le...
FIGURES | View All (13)
Journal Article
Published: 01 September 1973
Bulletin of Canadian Petroleum Geology (1973) 21 (3): 287–343.
... . An equivalent number of anhydrite to halite or occasionally dolomite to halite cycles were deposited under more restricted conditions in the La - Crete area. Major salt solution and/or differential compaction appea r to have taken place in Late Upper Muskeg time, which resulted in thickened Upper Muskeg...
Journal Article
Published: 01 December 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (4): 289–314.
... les années 1800 (Joggins Section). La nomenclature stratigraphique appliquée aux couches du Carbonifère supérieur, dont l’épaisseur excède localement 7 km, est problématique à cause de nombreuses unités mal définies ou officieuses et d’un mélange de terminologies litho-, bio-, et chrono...
Journal Article
Published: 01 June 1989
Canadian Journal of Earth Sciences (1989) 26 (6): 1089–1100.
... résultent de la submergence partielle d'une topographie complexe envahie par les dépôts de sédiments, et de l'existence de courants d'eau douce différentiels (à partir de la crête exposée de Port au Port) responsables de salinités fluctuantes et d'apports variables de silicoclastites. Les séquences de...
Image
Plots of ( a ) S2 vs. TOC and ( b ) OI vs. HI for Keg River Formation sampl...
Published: 01 March 2001
Fig. 4. Plots of ( a ) S2 vs. TOC and ( b ) OI vs. HI for Keg River Formation samples from the La Crete Subbasin.
Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2014
DOI: 10.1036/13431860M1063611
EISBN: 9781629812663
... , modified). 100 km (62.1 mi). Two regional NW-SE oriented crustal profiles from Crete to Egypt and Jordan ( Bentham et al., 2007 ) show clearly the oceanic nature of the Herodotus Basin and the sharp transition to continental crust below the Egyptian Margin. A better understanding...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2011
GSA Bulletin (2011) 123 (11-12): 2115–2141.
... of the older basin strata. These processes led to the development of subbasins with lateral variations in basement topography, strata thickness, and sedimentary facies distribution, and generated a segmented basin architecture. High-angle synthetic and antithetic faults that formed extensively after 3 Ma...
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Image
Saturate fraction gas chromatograms of Keg River Formation samples from the...
Published: 01 March 2001
Fig. 5. Saturate fraction gas chromatograms of Keg River Formation samples from the La Crete Subbasin: a) Lower Keg River Member organic-rich interval from 3-15-10-71W5, depth 3195.5 ft. b) Upper Keg River Member organic-rich interval from 1-28-10-75W5, depth 2475.0 ft. For peak annotations
Journal Article
Journal: GSA Bulletin
Published: 01 March 2012
GSA Bulletin (2012) 124 (3-4): 499–516.
... and carbon isotopic compositions of carbonate from latest Messinian deposits along a W-E Mediterranean transect from southern Spain to Crete exhibit large variations, with dominantly low δ 18 O values indicating freshwater dilution ( Pierre et al., 2006 ). In the Northern Apennines, stable isotope signatures...
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Journal Article
Published: 13 August 2020
Geological Magazine (2021) 158 (4): 583–597.
FIGURES | View All (11)
Journal Article
Journal: Geosphere
Published: 01 December 2015
Geosphere (2015) 11 (6): 2067–2129.
...., 2010 ; Graindorge et al., 2008 ). The outer forearc is sedimentologically isolated from northern Sumatra by a longitudinal forearc basin, which is composed of the Aceh, Simeulue, Nias, Pini, Siberut, and Bengkulu Neogene forearc subbasins ( Matson and Moore, 1992 ; Sieh and Natawidjaja, 2000...
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Journal Article
Published: 01 March 2001
Bulletin of Canadian Petroleum Geology (2001) 49 (1): 117–148.
...Fig. 4. Plots of ( a ) S2 vs. TOC and ( b ) OI vs. HI for Keg River Formation samples from the La Crete Subbasin. ...
FIGURES | View All (22)
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2004
DOI: 10.1144/GSL.SP.2004.221.01.07
EISBN: 9781862394698
...) is distinguished and located in the eastern part of the Annot subbasin where the thicker and coarser turbidites are confined to the St-Benoit area, eastward to the Rouaine fault-zone. The turbidite sedimentation continues with lobe-system deposition (the Crete de la Barre upper member), bounded at the base...
Journal Article
Journal: GSA Bulletin
Published: 29 March 2021
GSA Bulletin (2021)
... carbonate precipitation-sedimen- tation in the context of an overfilled lake basin (Marsicano et al., 2010; Mancuso and Caselli, 2012). Moreover, the Los Rastros system is un- usual in that the carbonates are preserved on the active margin of the subbasin, whereas car- bonate lake facies models suggest...