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Nukhul Formation

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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2013
GeoArabia (2013) 18 (4): 137–174.
... focused on the poorly dated Nukhul Formation, for which very little information from palynology is available despite its importance from a petroleum viewpoint. The assemblages discovered in our study are moderately preserved and reveal a sparse but significant record of spores and pollen...
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Journal Article
Published: 01 July 2013
Journal of Micropalaeontology (2013) 32 (2): 183–195.
...Haytham El Atfy; Rainer Brocke; Dieter Uhl Abstract Moderately to well-preserved palynomorph assemblages were recorded from thirty samples of the Nukhul Formation (GH 404-2A Well), southern Gulf of Suez, Egypt. The taxa are dominated by highly diverse fungi, freshwater algae (e.g. Botryococcus...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2012
GeoArabia (2012) 17 (1): 103–120.
...Abdel Galil A. Hewaidy; Sherif Farouk; Haitham M. Ayyad ABSTRACT The Nukhul Formation is the oldest syn-rift rock unit in the Gulf of Suez rift system in Egypt. The age of the formation is inadequately resolved by biostratigraphy and it is generally assigned to the Lower Miocene by stratigraphic...
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Journal Article
Published: 01 May 2003
Journal of Sedimentary Research (2003) 73 (3): 407–420.
...Ian D. Carr; Rob L. Gawthorpe; Christopher A.L. Jackson; Ian R. Sharp; Ali Sadek Abstract Facies and tectono-stratigraphic models for the tidally influenced Miocene Nukhul Formation are presented, based on outcrop data from Hammam Faraun fault block, Suez Rift, Egypt. Deposits of the Nukhul...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 2001
AAPG Bulletin (2001) 85 (10): 1871–1890.
...Robert D. Winn, Jr.; Paul D. Crevello; William Bosworth Abstract The Aquitanian-early Burdigalian (lower Miocene) Nukhul Formation at Gebel el Zeit, Egypt, was deposited during early stages of Gulf of Suez rifting. The unit dips 8-15° less than underlying prerift strata, indicating that significant...
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Journal Article
Published: 01 January 1987
Journal of Foraminiferal Research (1987) 17 (1): 74–91.
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Type section of the <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span> in Wadi <span class="search-highlight">Nukhul</span> (reproduced from  Wesco...
Published: 01 January 2012
Figure 6: Type section of the Nukhul Formation in Wadi Nukhul (reproduced from Wescott et al., 1996 ; Krebs et al., 1997 ). In the present paper the base of the formation is named the Suez Rift Unconformity; continental Unit 1 and near-shore Unit 2 are correlated to the Shoab Ali Member
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Stratigraphic schemes for the <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span> discussed in the paper. The ...
Published: 01 January 2012
Figure 3: Stratigraphic schemes for the Nukhul Formation discussed in the paper. The present study follows Saoudi and Khalil (1986) and Richardson and Arthur (1988) and divides the Nukhul Formation into the continental clastics of the Shoab Ali Member, and the Upper Nukhul members consisting
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A)  Location map indicating studied exposures of the <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span> in th...
Published: 01 May 2003
Figure 1 A) Location map indicating studied exposures of the Nukhul Formation in the Hammam Faraun fault block, Western Sinai, Gulf of Suez, and locations of other figures in this paper. Paleocurrents (insets) from the Thal and Tanka areas show NW-SE oriented tidal cross-beds and NNE oriented
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(a) Stratigraphy of the <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span> and Rudeis-Kareem interval, North ...
Published: 01 October 2001
Figure 15 (a) Stratigraphy of the Nukhul Formation and Rudeis-Kareem interval, North Gebel el Zeit See Figure 4 for locations of described sections NGZ-1, NGZ-2, and NGZ-3 and cross faults. NGZ-4 is located 1.75 km north of NGZ-3. NGZ-5 is 3.4 km north of NGZ-4. NGZ-A is located 0.5 km south
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Lithologic and electric logs of the <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span> within the studied wel...
Published: 01 October 2013
Figure 2: Lithologic and electric logs of the Nukhul Formation within the studied wells, Gulf of Suez, Egypt (modified after GUPCO, 1983 , 1986 ).
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A tentative ecological model during the deposition of the <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span> ...
Published: 01 October 2013
Figure 6: A tentative ecological model during the deposition of the Nukhul Formation (not to scale).
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Lithological log of the <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span>, GH 404-2A Well, Gulf of Suez, Egy...
Published: 01 July 2013
Fig. 2. Lithological log of the Nukhul Formation, GH 404-2A Well, Gulf of Suez, Egypt, modified after GUPCO ( 1983 ). The OMB is placed tentatively at the lithological boundary between the Shoab Ali and Ghara members ( Hewaidy et al. , 2012 , and this study). According to sequence stratigraphy
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Fungal palynomorphs from the <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span>, GH 404-2A Well, Gulf of Suez...
Published: 01 July 2013
Explanation of Plate 1. Fungal palynomorphs from the Nukhul Formation, GH 404-2A Well, Gulf of Suez, Egypt: monocellate fungal spores. fig. A. Exesisporites annulatus ; GH04-174-1; EF X35-1. fig. B. Exesisporites neogenicus ; GH04-176-1; EF B31-1. fig. C. Inapertisporites sp.; GH04-174-1
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Fungal palynomorphs from the <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span>, GH 404-2A Well, Gulf of Suez...
Published: 01 July 2013
Explanation of Plate 2. Fungal palynomorphs from the Nukhul Formation, GH 404-2A Well, Gulf of Suez, Egypt. figs A–F. Dicellate fungal spores: A , Dicellaesporites inaequabilis ; GH04-176-1; EF Y52-1; B , Dicellaesporites keralensis ; GH04-174-1; EF P30-1; C , Dyadosporites solidus ; GH04
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Fungal palynomorphs from the <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span>, GH 404-2A Well, Gulf of Suez...
Published: 01 July 2013
Explanation of Plate 3. Fungal palynomorphs from the Nukhul Formation, GH 404-2A Well, Gulf of Suez, Egypt. figs A–G. Fungal fruiting bodies: A , Polycellaesporonites acuminatus ; GH04-158-1; EF O61-4; B , Reduviasporonites cf. qingfengensis ; GH04-168-2;K EF X51-4; C , Phragmothyrites
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Composite section of the <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span> showing its four members (reprodu...
Published: 01 January 2012
Figure 4: Composite section of the Nukhul Formation showing its four members (reproduced from Saoudi and Khalil, 1986 ). Note the boundaries between the Shoab Ali Member and the Upper members are not defined in the same wells or outcrops. In the present paper the base of the oldest syn-rift
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Thickness of the <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span> as contoured by  Richardson and Arthur (1...
Published: 01 January 2012
Figure 8: Thickness of the Nukhul Formation as contoured by Richardson and Arthur (1988) .
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Thickness of (a) <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span>, and (b) Lower Rudeis Member (Mheiherrat ...
Published: 01 January 2012
Figure 9: Thickness of (a) Nukhul Formation, and (b) Lower Rudeis Member (Mheiherrat Formation) in the area of the October and North October oil fields (see Figure 2 for location; reproduced from Dolson et al., 1996 ). The Nukhul Formation and Lower Rudeis Member are absent over the crest
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A)  Genetic facies model for the <span class="search-highlight">Nukhul</span> <span class="search-highlight">Formation</span>, based on outcrops from t...
Published: 01 May 2003
Figure 3 A) Genetic facies model for the Nukhul Formation, based on outcrops from the Hammam Faraun block. Offshore to shoreface (Facies Association A) deposits trace laterally to estuary deposits (Facies Associations B-D). B) Schematic longitudinal cross section, based on outcrops from