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Mamuniyat Formation

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Typical outcrop of the Mamuniyat Formation in Jabal Eghei, where the formation is exclusively dominated by sandstone. (a) Humpback dunes overlain by antidunes, suggesting a waning flow signature during a jökulhlaup glacial flood (Lang & Winsemann 2013). (b) Chute and pool structures, capped by antidunes, implying a waning flow signature. These sedimentary structures are very typical of deposits of the Hirnantian glacial maximum, with broadly comparable facies recognized from southern Algeria, western Libya (Girard et al. 2012) and the Libyan–Egyptain border (Le Heron et al. 2010).
Published: 01 March 2013
Fig. 3. Typical outcrop of the Mamuniyat Formation in Jabal Eghei, where the formation is exclusively dominated by sandstone. ( a ) Humpback dunes overlain by antidunes, suggesting a waning flow signature during a jökulhlaup glacial flood ( Lang & Winsemann 2013 ). ( b ) Chute and pool
Journal Article
Published: 01 March 2013
Journal of the Geological Society (2013) 170 (2): 327–339.
...Fig. 3. Typical outcrop of the Mamuniyat Formation in Jabal Eghei, where the formation is exclusively dominated by sandstone. ( a ) Humpback dunes overlain by antidunes, suggesting a waning flow signature during a jökulhlaup glacial flood ( Lang & Winsemann 2013 ). ( b ) Chute and pool...
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First thumbnail for: Did lingering ice sheets moderate anoxia in the Ea...
Second thumbnail for: Did lingering ice sheets moderate anoxia in the Ea...
Third thumbnail for: Did lingering ice sheets moderate anoxia in the Ea...
Journal Article
Journal: AAPG Bulletin
Published: 15 September 2019
AAPG Bulletin (2019) 103 (9): 2219–2246.
... Paleozoic succession comprises the terrigenous Cambrian–Ordovician Gargaf Group consisting of at least five formations; from bottom to top, they are the following: Hasawnah, Ash Shabiyat, Hawaz, Melaz Shuqran, and Mamuniyat Formations ( Figure 2 ). The lowermost Hasawnah Formation rests unconformably...
FIGURES
First thumbnail for: Sedimentology of a “nonactualistic” Middle Ordovic...
Second thumbnail for: Sedimentology of a “nonactualistic” Middle Ordovic...
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Ordovician-Silurian contact exposed in section Ghat-6 (a) and Ghat-7 (b) (see Figure 2 for location map). The vehicles stand on sandstones of the upper Ordovician Mamuniyat Formation, while the hills are formed by the basal part of the Silurian Tanezzuft shales. In section Ghat-7 (b) the exposed shales are capped by a volcanic rock unit. (c) Typical red and green colours of the Silurian hot shale in the Ghat outcrop belt (section Ghat-3). (d) Close-up of the contact between Ordovician Mamuniyat Formation sandstones and Silurian Tanezzuft shales in section Ghat-3.
Published: 01 July 2006
Figure 7: Ordovician-Silurian contact exposed in section Ghat-6 (a) and Ghat-7 (b) (see Figure 2 for location map). The vehicles stand on sandstones of the upper Ordovician Mamuniyat Formation, while the hills are formed by the basal part of the Silurian Tanezzuft shales. In section Ghat-7 (b
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Basal sandy carbonate facies association. (a) Relationship between the topmost part of the Mamuniyat Formation and the Tanezzuft Formation in Jabal Eghei. The basal sandy carbonate facies association fills in hollows on the topmost surface of the Mamuniyat Formation sandstones beneath. This contact is clearly marked on the measured section in Figure 4, which encompasses all strata visible in this photograph. The Tanezzuft Formation forms the generally recessive topography in the middle distance to background, which is capped disconformably by the ‘Nubian Sandstone’ of probable Jurassic age (see Fig. 2 for chronostratigraphy). (b) Bioturbated, quartz-bearing grainstone. (c) Mottled grainstone to floatstone with clearly visible crinoid ossicles among the shell fragments. Pencil 5 cm long.
Published: 01 March 2013
Fig. 5. Basal sandy carbonate facies association. ( a ) Relationship between the topmost part of the Mamuniyat Formation and the Tanezzuft Formation in Jabal Eghei. The basal sandy carbonate facies association fills in hollows on the topmost surface of the Mamuniyat Formation sandstones beneath
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Chronostratigraphy of the studied succession on Jabal Eghei, where four stratigraphic units are recognized. These comprise, in ascending stratigraphic order, the Hawaz, Mamuniyat and Tanezzuft formations and the Mesozoic sandstone (‘Nubian Sandstone’). Age constraints on the Hawaz Formation and ‘Nubian Sandstone’ are limited, but lithostratigraphic comparisons coupled with fossil occurrences, including wood fragments in the latter unit, allow Middle Ordovician and Jurassic ages to be assigned respectively (e.g. Bellini et al. 1991). The Mamuniyat Formation similarly is ill constrained in Jabal Eghei, whereas the Tanezzuft Formation contains graptolites of Hirnantian–Rhuddanian affinity (Page et al. 2013).
Published: 01 March 2013
Fig. 2. Chronostratigraphy of the studied succession on Jabal Eghei, where four stratigraphic units are recognized. These comprise, in ascending stratigraphic order, the Hawaz, Mamuniyat and Tanezzuft formations and the Mesozoic sandstone (‘Nubian Sandstone’). Age constraints on the Hawaz
Journal Article
Journal: Interpretation
Published: 30 August 2016
Interpretation (2016) 4 (4): T507–T519.
... Shuqran Formations were deposited to fill the paleovalleys during Later-Ordovician glacial events. The top of the Mamuniyat was eroded and overlaid by Bir Tlacsin in some area and by thick shale of Tanezzuft Formation elsewhere, which formed the hydrocarbon seal and source rock at the base...
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First thumbnail for: Using instantaneous frequency and colored inversio...
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Newly recognized glacial features within the Tanezzuft Formation of Jabal Eghei. The stratigraphic position of these features is shown in Figure 4. (a) Soft-sediment striated surface, comprising streamlined ridges and grooves similar to those described elsewhere in Al Kufrah Basin within the Mamuniyat Formation (e.g. Le Heron & Howard 2010; Le Heron et al. 2010). (b) Circular concretions overgrowing and crosscutting the striations allow the hypothesis that the grooves are aeolian to readily be dismissed. (c) Further detail of striated surface, showing local evidence for crosscutting striations. (d) Micritic lonestone ‘floating’ within a siltstone bed, tentatively interpreted as a dropstone. Pencil 5 cm long.
Published: 01 March 2013
within the Mamuniyat Formation (e.g. Le Heron & Howard 2010 ; Le Heron et al . 2010 ). ( b ) Circular concretions overgrowing and crosscutting the striations allow the hypothesis that the grooves are aeolian to readily be dismissed. ( c ) Further detail of striated surface, showing local evidence
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Figure 3. Examples of landforms diagnostic of past glacial activity in Late Ordovician sediments of North and South Africa. A: Fluted soft-sediment striated surface at the top of the Late Ordovician Peninsula Formation, Pakhuis Pass, South Africa. Note circled person for scale. B: Detail of berms and furrows with parallel striations on fluted soft-sediment surface at the top of the Late Ordovician Peninsula Formation, Pakhuis Pass, South Africa. C: Detail of ridge with associated cross-fractures on fluted soft-sediment striated surface in the Late Ordovician Tamadjert Formation, Dider, Algeria, North Africa. Photograph is ∼2 m across. D: Detail of soft-sediment striated surface within the Late Ordovician Mamuniyat Formation, Gargaf Arch, Libya, North Africa.
Published: 01 April 2007
Africa. Photograph is ∼2 m across. D: Detail of soft-sediment striated surface within the Late Ordovician Mamuniyat Formation, Gargaf Arch, Libya, North Africa.
Journal Article
Published: 13 November 2009
Geological Magazine (2010) 147 (1): 28–41.
... the Melaz Shuqran and Mamuniyat formations, respectively, were published by El-ghali ( 2005 ). Logs from both of these wells are reproduced herein on Figure 5 . Both wells were drilled in the NC174 concession rather than NC115 ( Fig. 1 ). Figure 5 Sedimentary logs from the subsurface of the N...
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Cross section of the seven basal Silurian shale sections studied (see Figure 2 for location of sections; no horizontal scale implied). Using a cut-off of 10 ppm, the Silurian hot shale appears to be largely absent in two of the sections (Ghat-4 and Ghat-6), while maximum thicknesses of 12–13 m are reached in sections Ghat-3 and Ghat-7. The largest uranium concentrations were measured in sections Ghat-2 and Ghat-7 with values around 50 ppm. Topography interpreted based on lateral pinch-outs of of Mamuniyat Formation and hot shale. “Correlation datum” lies in the organically lean, “cold” shale.
Published: 01 July 2006
of 12–13 m are reached in sections Ghat-3 and Ghat-7. The largest uranium concentrations were measured in sections Ghat-2 and Ghat-7 with values around 50 ppm. Topography interpreted based on lateral pinch-outs of of Mamuniyat Formation and hot shale. “Correlation datum” lies in the organically lean
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(a) Late Ordovician palaeogeographic reconstruction of West Gondwana, showing the approximate extent of a grounded ice sheet and the position of the ancient South Pole (after Scotese et al., 1999; Sutcliffe et al., 2000b). Blue arrows indicate direction of ice sheet advance.
Published: 01 April 2004
) Location and geological sketch-map of the Murzuq Basin, showing the location of the study area, the distribution of seismically defined palaeovalleys (ater Smart, 2000 ) and the area where oil fields occur in the Mamuniyat Formation. (c) LANDSAT image and (d) interpretative sketch of the Gargaf Arch
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2006
GeoArabia (2006) 11 (3): 101–118.
...Figure 7: Ordovician-Silurian contact exposed in section Ghat-6 (a) and Ghat-7 (b) (see Figure 2 for location map). The vehicles stand on sandstones of the upper Ordovician Mamuniyat Formation, while the hills are formed by the basal part of the Silurian Tanezzuft shales. In section Ghat-7 (b...
FIGURES
First thumbnail for: Identification of early Llandovery (Silurian) anox...
Second thumbnail for: Identification of early Llandovery (Silurian) anox...
Third thumbnail for: Identification of early Llandovery (Silurian) anox...
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2004
GeoArabia (2004) 9 (2): 137–160.
...) Location and geological sketch-map of the Murzuq Basin, showing the location of the study area, the distribution of seismically defined palaeovalleys (ater Smart, 2000 ) and the area where oil fields occur in the Mamuniyat Formation. (c) LANDSAT image and (d) interpretative sketch of the Gargaf Arch...
FIGURES
First thumbnail for: Sedimentary architecture of Upper Ordovician tunne...
Second thumbnail for: Sedimentary architecture of Upper Ordovician tunne...
Third thumbnail for: Sedimentary architecture of Upper Ordovician tunne...
Journal Article
Journal: AAPG Bulletin
Published: 01 September 2006
AAPG Bulletin (2006) 90 (9): 1309–1336.
... and Worsley (2000) . As in previous works (i.e., Boote et al., 1998 ), these authors consider the Lower Silurian hot shales of the Tanezzuft Formation ( Figure 2 ) as the source rocks, whereas the Upper Ordovician sandstones of the Mamuniyat Formation are regarded as the main reservoir, leading...
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First thumbnail for: Stratigraphy and sedimentology of the Middle Ordov...
Second thumbnail for: Stratigraphy and sedimentology of the Middle Ordov...
Third thumbnail for: Stratigraphy and sedimentology of the Middle Ordov...
Journal Article
Journal: Interpretation
Published: 15 March 2019
Interpretation (2019) 7 (2): T383–T408.
... hydrocarbon reservoir unit occurring in the Late Ordovician rocks known as the Mamuniyat Formation, which is the main sand-prone sedimentary package in the study area ( McDougall and Martin, 2000 ). The extension of the Late Ordovician ice sheet is defined on the basis of key evidence, such as striated...
FIGURES
First thumbnail for: Ordovician glacial paleogeography: Integration of ...
Second thumbnail for: Ordovician glacial paleogeography: Integration of ...
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Field view looking northwest and sketch showing the relationships between U1 and U2 at the top of the Hawaz Formation. MN and MS = Upper Ordovician Mamuniyat and Melaz Shuqran formations, respectively. HW.3 = top of the Hawaz Formation. See the location of this point in the geological map (Figure 12).
Published: 01 September 2006
Figure 4 Field view looking northwest and sketch showing the relationships between U1 and U2 at the top of the Hawaz Formation. MN and MS = Upper Ordovician Mamuniyat and Melaz Shuqran formations, respectively. HW.3 = top of the Hawaz Formation. See the location of this point in the geological
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It shows a vertical seismic slice (a) before and (b) after applying band-pass filter. The seismic data exhibit poor vertical resolution because they fail to separate Bir Tlacsin Formation (black dot) at the top of the reservoir. The pseudoreflector of the side-lobe effect as it shown by yellow arrow in (a) was eliminated in (b), causing appearance of the high contrast within the sandstone reservoir facies. In addition, the continuity of stratigraphic surfaces is slightly improved in the deeper section (green arrows). One-dimensional forward models at wells W03 and W04 support the presence of side-lobe artifacts on the original seismic data. TZ = Tanezzuft, HS = hot shale, CM = clean Mamuniyat, DM = dirty Mamuniyat, BT = Bir Tlacsin, and MS = Melaz Shuqran.
Published: 30 August 2016
Figure 4. It shows a vertical seismic slice (a) before and (b) after applying band-pass filter. The seismic data exhibit poor vertical resolution because they fail to separate Bir Tlacsin Formation (black dot) at the top of the reservoir. The pseudoreflector of the side-lobe effect as it shown
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Measured section straddling the Mamuniyat and Tanezzuft formations and the ‘Nubian Sandstone’ in Jabal Eghei. The curve to the right of the logged section shows gamma-ray values obtained using a GF-InstrumentsTM gamma-ray spectrometer on the outcrop, for 3 min count intervals. The U content is commonly taken as a direct and linear proxy for former total organic carbon enrichment (TOC) (e.g. Lüning & Kolonic 2003; Lüning et al. 2003). The curve does not illustrate that proxy TOC values were elevated at or near the base of the Tanezzuft Formation, as is observed elsewhere in North Africa, such as in the Ghat area of SW Libya (Lüning et al. 2003). A simple interpretation (high versus low) of relative sea level, ice and anoxia is also shown. This relative sea-level curve takes into account the progressive upsection loss of hummocky cross-stratification and increase in mud content, compatible with a deepening trend. Ice presence is interpreted on the basis of soft-sediment striae and/or lonestones and manganese oxide concretions. Anoxia is inferred on the basis of faunal preservation in the graptolite assemblage (Page et al. 2013), with more oxic conditions indicated by the presence of bioturbation and manganese nodules.
Published: 01 March 2013
Fig. 4. Measured section straddling the Mamuniyat and Tanezzuft formations and the ‘Nubian Sandstone’ in Jabal Eghei. The curve to the right of the logged section shows gamma-ray values obtained using a GF-Instruments TM gamma-ray spectrometer on the outcrop, for 3 min count intervals. The U
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The 946 ms interpreted time slice showing possible different depositional environments and distinguishing three likely sedimentation belts, X, Y, and Z. The black circles show the location of wells with relevant Melez Shuqran, Mamuniyat, or Bir Tlacsin drilled intervals. The corresponding environments that are interpreted range from subglacial to proglacial and more purely proglacial (most likely mainly Melaz Shuqran), to marginal marine (lower energy environment) to distal marine, which, in the case of this time slice, would correspond to the Tannezuft Formation filling up the accommodation space left basinward by the glacial system. In addition, some preserved terraces formed by the remnant sediment from a previous glacial advance and retreat are interpreted around some Hawaz paleohighs.
Published: 15 March 2019
Figure 20. The 946 ms interpreted time slice showing possible different depositional environments and distinguishing three likely sedimentation belts, X, Y, and Z. The black circles show the location of wells with relevant Melez Shuqran, Mamuniyat, or Bir Tlacsin drilled intervals