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Reggane Basin

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Journal Article
Journal: AAPG Bulletin
Published: 01 November 2003
AAPG Bulletin (2003) 87 (11): 1799–1822.
... and Reggane basin, with a heat flow of approximately 63–67 mW/m 2 and a crustal thickness of 55–60 km. These values are comparable to those for the eastern Saharan basins, where the intensity of the Triassic activation decreased considerably from north to south. The present-day thermal regime of the Ahnet...
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Journal Article
Published: 01 May 2006
Geological Magazine (2006) 143 (3): 269–299.
... of a Devonian basin and ridge system. This area includes a series of intracratonic basins along the northern margin of the West African Craton which consists (from W to E) of the Reggane Basin, Azel Matti Ridge, Ahnet Basin, Foum Belrem Ridge and Mouydir Basin. The depositional and palaeogeographic...
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Series: Geological Society, London, Petroleum Geology Conference Series
Published: 01 January 2010
DOI: 10.1144/0070707
EISBN: 9781862394131
..., separating the Illizi and Berkine basins in Algeria, has continuously grown during the Cambro-Ordovician, stopped rising during the Silurian, and grew again continuously during the Devonian. The Bled El-Mass High is a part of the Azzel-Matti Ridge separating the Ahnet and Reggane basins in Algeria. The high...
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Numerical modeling of the thermal regime in the lithosphere of the <span class="search-highlight">Reggane</span> ...
Published: 01 November 2003
Figure 5 Numerical modeling of the thermal regime in the lithosphere of the Reggane basin, well RPL-101. (A) Burial, thermal, and maturation histories. (B) Tectonic subsidence of the basement surface. (C) Thermal evolution of the lithosphere (the legend is similar to Figure 3B –D).
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W–E transect through the northern Ahnet–northern Mouydir from the <span class="search-highlight">Reggane</span> B...
Published: 01 May 2006
Figure 10. W–E transect through the northern Ahnet–northern Mouydir from the Reggane Basin (384) into the Mouydir Basin. Note extreme increase of Givetian thickness in the eastern Mouydir (376, 335). Continuous lines – biostratigraphic correlations; broken lines – lithostratigraphic correlations
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W–E transect through the northern Ahnet–northern Mouydir from the <span class="search-highlight">Reggane</span> B...
Published: 01 May 2006
Figure 10. W–E transect through the northern Ahnet–northern Mouydir from the Reggane Basin (384) into the Mouydir Basin. Note extreme increase of Givetian thickness in the eastern Mouydir (376, 335). Continuous lines – biostratigraphic correlations; broken lines – lithostratigraphic correlations
Journal Article
Published: 01 January 1960
Bulletin de la Société Géologique de France (1960) S7-II (5): 534–539.
...Andre Bonnet; J. Fabre; R. Feys Abstract Drilling for oil in the Reggan region (Algeria) of the western Sahara shows the presence of a Carboniferous basin, in which two continental series--Namurian and Stephanian--can be distinguished. The Westphalian is essentially absent. Some fossils (fish...
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Maturation and temperature profiles in the present-day section of the Timim...
Published: 01 November 2003
Figure 4 Maturation and temperature profiles in the present-day section of the Timimoun basin, well REG-1 (A, B, D) and the Reggane basin, well RPL-101 (C). (A) Calculated (lines) and measured (asterisks) present-day values of vitrinite reflectance (R o ). Solid line: R o computed from burial
Image
Schematic cross-section from the <span class="search-highlight">Reggane</span> into the Mouydir <span class="search-highlight">basin</span>, flattened ...
Published: 01 May 2006
Figure 16. Schematic cross-section from the Reggane into the Mouydir basin, flattened at the base of the uppermost Famennian Grès du Khenig, approximately along the transect of Figure 10 . Solid lines – chronostratigraphic boundaries; broken line – lithostratigraphic boundary. Legend
Series: Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP326.8
EISBN: 9781862395749
... maturation history may be unfavourable for the preservation of Infracambrian-sourced hydrocarbons in this area. Local development of Infracambrian source facies may also occur in the Reggane, Ahnet, Mouydir and Iullemeden basins, as indicated by black shales in wells MKRN-1 and MKRS-1 in the Ahnet Basin...
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Journal Article
Published: 01 September 2016
Russ. Geol. Geophys. (2016) 57 (9): 1342–1348.
... Atlas; 9, Algerian–Libyan; 10, Sahara–East Mediterranean; 11, Gulf of Suez depression of the Red Sea–Suez basin; 12, West Moroccan; 13, Aaiun; 14, Tindouf; 15, Reggane; 16, Murzuq; 17, Kufra; 18, Red Sea depression of the Red Sea–Suez basin; 19, Senegal; 20, Taoudeni; 21, Mali–Niger; 22, Chad; 23, Gao...
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Journal Article
Published: 01 January 1960
Bulletin de la Société Géologique de France (1960) S7-II (2): 240–262.
...Marie Louise Remack-Petitot Abstract Study of the rich conodont faunas recovered from numerous borings and sections in the Fort-Polignac, Reggane, and Bechar basins (Algeria) in the Sahara and of faunas from the Pyrenees and the Montagne Noire in France demonstrates the value of conodonts...
Journal Article
Published: 01 January 1960
Bulletin de la Société Géologique de France (1960) S7-II (2): 230–239.
...Marie Louise Remack-Petitot Abstract Certain details of the Gotlandian (Silurian) stratigraphy of the Sahara have been clarified on the basis of a rich graptolite fauna collected from borings and sections in the Reggane and Fort-Polignac basins (Algeria). It is established that datable lower...
Journal Article
Journal: AAPG Bulletin
Published: 11 October 1997
AAPG Bulletin (1997) 81 (10): 1679–1699.
... in the central and eastern parts of the Saharan platform and are investigated in detail. The Ahnet, Mouydir, Timimoun, Reggane, and other basins located in the southern and western parts of the platform are also studied. The modeling results, combined with geochemical data, are used in a synthesis...
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Series: Geological Society, London, Petroleum Geology Conference Series
Published: 01 January 2010
DOI: 10.1144/0070725
EISBN: 9781862394131
..., Morocco; NW Murzuk Basin, Libya) were logged for this study (Figs  1 & 2 ). All sections are located along the southern Palaeozoic outcrop belt, comprising exposures in the Anti-Atlas, the Bechar Basin, the Reggane, Ahnet and Mouydir Basins, the southern Illizi Basin, and the northern Murzuk...
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A , location of the main Carboniferous <span class="search-highlight">Basins</span> in Morocco, Algeria and Tunis...
Published: 01 November 2011
F igure 1 A , location of the main Carboniferous Basins in Morocco, Algeria and Tunisia: 1 , Central Massif; 2 , Rehamna; 3 , Djebilet; 4 , Tafilalt; 5 , Béchar; 6 , Jerada; 7 , Tindouf; 8 , Reggane; 9 , Ahnet; 10 , Mouydir; 11 , subsurface Carboniferous; AA = Anti-Atlas, ATF = Atlas
Journal Article
Journal: AAPG Bulletin
Published: 01 October 2003
AAPG Bulletin (2003) 87 (10): 1623–1651.
... sheets. Veins correspond to filling per ascensum of fractures and faults, their thickness ranges from 2 to 20 m, and they could be extended as much as 100 km. As to age, the dolerites are distributed over a wide time interval ( Conrad, 1972 ; Conrad and Westphal, 1975 ): 166 Ma in the Reggane basin, 166...
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Journal Article
Published: 01 November 2011
Journal of Paleontology (2011) 85 (6): 1105–1127.
...F igure 1 A , location of the main Carboniferous Basins in Morocco, Algeria and Tunisia: 1 , Central Massif; 2 , Rehamna; 3 , Djebilet; 4 , Tafilalt; 5 , Béchar; 6 , Jerada; 7 , Tindouf; 8 , Reggane; 9 , Ahnet; 10 , Mouydir; 11 , subsurface Carboniferous; AA = Anti-Atlas, ATF = Atlas...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1958
AAPG Bulletin (1958) 42 (7): 1631–1679.
.... of new concessions in 5 blocks which are mainly situated in the northern Sahara on acreage recently released by SN REPAL and CFPA. Exploration .—In the Adrar sector a party of 2 geologists is assigned to the detailed study of the borders of the Reggane basin and the investigation of isolated...
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Map of Africa’s sedimentary <span class="search-highlight">basins</span> with discovered and yet-to-find oil and ...
Published: 01 September 2016
, Western Tell; 3, Southern Tell; 4, Eastern Tell; 5, Eastern Atlas; 6, Tunisia–Sicily; 7, Middle Atlas; 8, Central Atlas; 9, Algerian–Libyan; 10, Sahara–East Mediterranean; 11, Gulf of Suez depression of the Red Sea–Suez basin; 12, West Moroccan; 13, Aaiun; 14, Tindouf; 15, Reggane; 16, Murzuq; 17, Kufra