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Mouydir Basin

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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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(A) WSW-ENE geological cross section of the <span class="search-highlight">Mouydir</span> <span class="search-highlight">Basin</span> showing typical a...
Published: 02 April 2021
Fig. 3 (A) WSW-ENE geological cross section of the Mouydir Basin showing typical arch and basin architecture defined as a syncline-shaped basin with boundary secondary arches. (B) NW-SE seismic profiles of the Ahnet Basin defined as a complex shaped basin with intra-basin arches. The specific
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Schematic cross-section from the Reggane into the <span class="search-highlight">Mouydir</span> <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
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(A) Geological map of the Ahnet and the <span class="search-highlight">Mouydir</span> <span class="search-highlight">Basins</span> modified from  Perro...
Published: 02 April 2021
Fig. 2 (A) Geological map of the Ahnet and the Mouydir Basins modified from Perron et al. , (2018) showing the specific zonation of the terranes, the paleocurrents directions (from Beuf et al. , 1971 ) and the evidence of sedimentary structures on arches (from Perron et al. , 2018 ; Wendt
Journal Article
Journal: AAPG Bulletin
Published: 01 November 2003
AAPG Bulletin (2003) 87 (11): 1799–1822.
.... The modeling shows that thermal activation during the Permian–Triassic–Jurassic was most intense in the Timimoun basin and the northern part of the Ahnet and Mouydir basins, with a heat flow of about 70–80 mW/m 2 and a lithosphere thickness of 40–50 km. Activation was more moderate in the Sbaa subbasin...
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W–E transect through the northern Ahnet–northern <span class="search-highlight">Mouydir</span> from the Reggane 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 <span class="search-highlight">Mouydir</span> from the Reggane 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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Comparison of total subsidence curves between numerical models and geologic...
Published: 02 April 2021
Fig. 12 Comparison of total subsidence curves between numerical models and geological data extracted from the Mouydir Basin, Algeria (9: Well W21; Perron et al. , 2018 ) and the Ahnet Basin, Algeria (5: well W1, Kracha, 2011 ). The Algerian wells are localized in Figure 2A . The curves
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Compilation of total burial subsidence of intracratonic <span class="search-highlight">basins</span> modified fro...
Published: 02 April 2021
, Algeria, well W1 ( Kracha, 2011 ); 6: Ghadames/Berkine Basin, Algeria ( Yahi, 1999 ); 7: Illizi Basin well, Algeria ( Wells et al. , 2018 ); 8: Mouydir Basin, Algeria Well W21 ( Perron et al. , 2018 ); 9: Tyumen SG-6 section, Urengoy region, Russia ( Nikishin et al. , 2002 ); 10: North Dakota
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Ternary classification of low rate intracratonic <span class="search-highlight">basins</span>. The diagram relate...
Published: 02 April 2021
to their architecture, geometry and subsidence history (see Fig. 12 ): 1: Ahnet Basin, North Africa ( Perron et al. , 2018 ); 2: Mouydir Basin, North Africa ( Perron et al. , 2018 ); 3: Tim Mersoï Basin, North Africa ( Perron, 2019 ); 4: Tamesna Basin, North Africa ( Lessard, 1961 ; Perron, 2019 ). Notice that here
Journal Article
Published: 02 April 2021
Bulletin de la Société Géologique de France (2021) 192 (1): 15.
...Fig. 3 (A) WSW-ENE geological cross section of the Mouydir Basin showing typical arch and basin architecture defined as a syncline-shaped basin with boundary secondary arches. (B) NW-SE seismic profiles of the Ahnet Basin defined as a complex shaped basin with intra-basin arches. The specific...
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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, 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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Upper Silurian (Lower Ludlow) facies distribution of the Fegaguira Formatio...
Published: 11 September 2023
and argillaceous-calcareous facies. To the south in the different basins (Ahnet, Mouydir, illizi and Berkine–Ghadames), the Upper Silurian deposits are dominantly represented by sandy facies recording a major progradation. This is well illustrated in the southern parts of the Ilizi and Berkine–Ghadames basins
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1971
AAPG Bulletin (1971) 55 (8): 1295–1335.
... the northern Ahaggar crystalline basement complex southeastward to Djado at the south end of the Murzuk basin. The rocks, which are mainly quartzite, sandstone, sandy mudstone, and conglomerate, in the southern part of the area are generally reduced to a tenth of the maximum thickness prevailing in the Chaînes...
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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 December 1987
AAPG Bulletin (1987) 71 (12): 1445–1466.
... rocks was about 100°C in the early Tertiary, and wet gas in the northeastern and southwestern parts of the basin, where maximum temperature reached about 130°C. To the west, the Ahnet and Mouydir basins contain the same sequence of source rocks, but their temperature reached 130°-160°C in the Ahnet...
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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: Interpretation
Published: 17 April 2024
Interpretation (2024) SE25–SE33.
... perimeter, the central part of the Oued Mya Basin (Figure  1 ), which is north–south to northeast–southwest elongated cratonic basin in Saharan Algeria. The Touggourt saddle is situated in the north, whereas a structural terrace separates the Oued Mya Basin from the Mouydir Basin in the south. The basin has...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1971
AAPG Bulletin (1971) 55 (12): 2225–2245.
... of the paleoclimatic, paleostructural, and paleogeographic agents that controlled the detrital sedimentation. For this kind of fundamental study and to obtain a better knowledge of the oil reservoir characteristics and their lateral variations in the basins, the Sahara proved a very favorable area. 1...
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