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Ghara Member

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Cumulative thickness of the anhydrite beds in the <b>Ghara</b> <b>Member</b> of the Nukhu...
Published: 01 January 2012
Figure 10: Cumulative thickness of the anhydrite beds in the Ghara Member of the Nukhul Formation (reproduced from Saoudi and Khalil, 1986 ).
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2012
GeoArabia (2012) 17 (1): 17–44.
...Figure 10: Cumulative thickness of the anhydrite beds in the Ghara Member of the Nukhul Formation (reproduced from Saoudi and Khalil, 1986 ). ...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2013
GeoArabia (2013) 18 (4): 137–174.
... assumed to be representatives for this period on a regional scale. In addition, the Oligocene/Miocene Boundary (OMB) could be lithostratigraphically defined within the studied formation, most likely at the boundary between the lower Shoab Ali Member and upper Ghara Member. A fungal/algal ‘event’ within...
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Image
Cross-sections AA′, BB′ and CC′ in the southern Gulf of Suez showing the Sh...
Published: 01 January 2012
Figure 5: Cross-sections AA′, BB′ and CC′ in the southern Gulf of Suez showing the Shoab Ali and Ghara members of the Nukhul Formation (reproduced from Saoudi and Khalil, 1986 ). In the cross-section CC′ in Figure 5c the four anhydrite marker beds are interpreted to merge into Marker 1
Image
Location map of the studied well (GH 404-2A), the type section of the Nukhu...
Published: 01 July 2013
Fig. 1. Location map of the studied well (GH 404-2A), the type section of the Nukhul Formation (Wadi Nukhul) and the type wells of the Shoab Ali and Ghara members, Gulf of Suez, Egypt. Map based mainly on GUPCO (1983).
Image
Lithology of the Nukhul Sequence in the Wadi Dib-1 Well as described by Che...
Published: 01 January 2012
Figure 12: Lithology of the Nukhul Sequence in the Wadi Dib-1 Well as described by Chevron’s well site geologists M. Raslan, C. Allen and Z. Ebeid. Six Nukhul shale-sandstone subsequence are here interpreted in the Shoab Ali Member between 11,602–10,586 ft. The Ghara Member occurs between 10,586
Image
Lithological log of the Nukhul Formation, 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
Journal Article
Published: 01 July 2013
Journal of Micropalaeontology (2013) 32 (2): 183–195.
...Fig. 1. Location map of the studied well (GH 404-2A), the type section of the Nukhul Formation (Wadi Nukhul) and the type wells of the Shoab Ali and Ghara members, Gulf of Suez, Egypt. Map based mainly on GUPCO (1983). ...
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Stratigraphic schemes for the Nukhul Formation discussed in the paper. The ...
Published: 01 January 2012
of the October (mainly clastics), Ghara (mainly evaporites) and Gharamul (mainly carbonates) members.
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The Nukhul Sequence is calibrated in the present study between ca. 25.0 and...
Published: 01 January 2012
Member to the marine Upper Nukhul members (Ghara and Gharamul) at ca. 22.6 Ma. The figure shows radiometric dates for basalts, strontium age for the Yanbu Salt and biostratigraphic assignments.
Journal Article
Published: 16 January 2020
The Canadian Mineralogist (2020) 58 (1): 71–83.
... 3000 years BC ( Garazhian & Lotfi-Gharae 2015 , Basafa 2016 ). Turquoise has many mineral simulants. Some of these, such as faustite, chalcosiderite, and planerite, belong to the turquoise group ( Foord & Taggart 1998 , Murthy 1989 ), but others, such as variscite, amazonite (a variety...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2009
GeoArabia (2009) 14 (4): 139–162.
... to the southern Gulf: (1) continental clastics of the October Member, (2) alternating marls and evaporites of the Ghara Member, and (3) carbonates of the Gharamul Member. The thickness of the Nukhul Formation varies considerably due to syn-depositional faulting and ranges from zero to 800 m. Above the Nukhul...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1988
AAPG Bulletin (1988) 72 (10B): 321–342.
...), whereas surface exploration and drilling decreased significantly (about 30% and 20%, respectively, from 1986 levels). The two OPEC-member countries adhered to imposed quotas, recording somewhat lower production levels in 1987 than in 1986; however, total production of the North Africa countries increased...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1996
AAPG Bulletin (1996) 80 (1): 101–118.
... member (Ghara Member) consists of anhydrite (indicating deposition in a supratidal/sabkha setting), shallow-marine limestones and shales (suggesting shallow shelf deposition), and continental sandstone (representing subaerial deposition) ( Figure 3 ). Khalil and Meshref (1988) suggested two phases...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 2003
AAPG Bulletin (2003) 87 (1): 143–180.
... Holocene coastal sabkhas of the Arabian Gulf region and the geology and hydrocarbon habitats of the Middle East and North Africa. He is a member of the AAPG, SEPM, International Association of Sedimentologists, and Geological Society of London. Interbedded Oligocene limestones, sandstones...
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Journal Article
Journal: AAPG Bulletin
Published: 11 October 1997
AAPG Bulletin (1997) 81 (10): 1640–1659.
...-Miocene sequences. The upper member (Ghara) consists of anhydrites, limestones, shales, and sandstones deposited in restricted shallow-marine and continental settings ( Figure 4 ) ( Saoudy and Khalil, 1984 ). Because the maximum extensional stresses resulted in rapid subsidence, major half-graben...
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Journal Article
Published: 01 September 1994
Bulletin of Canadian Petroleum Geology (1994) 42 (3): 312–331.
... in a lagoonal to shallow marine setting. It is subdivided into four members in ascending order: Baba, Sidri, Feiran and Hammam Faraun. 1. Baba Member: This is composed mainly of anhydrite with subordinate shale. The member ranges in thickness from 14 to 81 m in the southern Gulf of Suez. 2. Sidri Member...
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 1999
GeoArabia (1999) 4 (4): 503–542.
... region of western Saudi Arabia. Regional Equivalents: Ghara Member of the Nukhul Formation ( Saoudi and Khalil, 1984 ) in the Gulf of Suez and Egyptian Red Sea; and subsurface in the Yemeni and Somali Gulf of Aden ( Hughes and Beydoun, 1992 ). Type Section: Saudi Aramco exploration wells near...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2005
GeoArabia (2005) 10 (3): 49–126.
... is not exposed in the Saudi Arabian Red Sea region. Name: Hughes and Filatoff (1995) named the Yanbu Formation for a subsurface succession of evaporites in the Yanbu region of western Saudi Arabia ( Figure 1c ). Regional Equivalents: The Yanbu Formation is correlated to the Ghara Member...
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Journal Article
Published: 01 January 1971
Journal of the Geological Society (1971) 127 (1): 69–93.
... of hazel, with Vallonia costata s a characteristic member of the biotope. Pomatias elegans, Azeca menkeana, Clausilia pumila, Vertigo pusilla and Ena montana would belong in this habitat. The relative scarcity of Zonitidae and of Discus rotundatus argues against a heavy forest cover, and Azeca is a wood...