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Sudr Chalk

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Figure 1. Location (inset) and geology of Gebel El Minshera, modified from the Geological Survey of Egypt (1993). Formations cropping out at Gebel El Minshera are assigned the following ages and nomenclature by Issawi et al. (2009): Safa (Bathonian), Malha (Early Cretaceous), Galala (Cenomanian), Wata (Turonian), and Matulla (Santonian). Surrounding post-Santonian deposits belong primarily to the Duwi Formation (Campanian) and Sudr Chalk (Maastrichtian–Danian) but also include the Esna (upper Paleocene–lower Eocene) and Thebes (lower Eocene) Formations. Previous biostratigraphic studies of the Malha and Galala Formations have been conducted in the Eastern Desert and Gulf of Suez and elsewhere on the Sinai Peninsula.
Published: 01 August 2010
), Wata (Turonian), and Matulla (Santonian). Surrounding post-Santonian deposits belong primarily to the Duwi Formation (Campanian) and Sudr Chalk (Maastrichtian–Danian) but also include the Esna (upper Paleocene–lower Eocene) and Thebes (lower Eocene) Formations. Previous biostratigraphic studies
Journal Article
Published: 20 April 2022
Journal of Foraminiferal Research (2022) 52 (2): 75–91.
... into: (Sudr Chalk, Esna Shale, and a massive Limestone). These formations were dated as Campanian and/or Maastrichtian for the Sudr Chalk, Danian and/or Paleocene for the Esna Shale, and lower Eocene for the upper limestone formation. Also, they decided that during the Late Cretaceous-Early Tertiary, great...
Journal Article
Published: 01 October 2001
Journal of Foraminiferal Research (2001) 31 (4): 385–388.
... throughout Sinai Peninsula and represented by Sudr Chalk Formation. This formation contains a rich fauna of planktonic and benthonic foraminifera, in addition to nannoplankton. Three sections were measured in west central Sinai; Gebel Bodhiya, Abu Zeneima-Wadi Nukhul range and Gebel Nezzazat covering...
Journal Article
Published: 01 September 1994
Bulletin of Canadian Petroleum Geology (1994) 42 (3): 312–331.
... deposited in a marine, inner sublittoral to littoral setting. CAMPANIAN-MAASTRICHTIAN SUCCESSION These are the youngest Cretaceous sedimentary ocks in the stratigraphic section. They consist of two formations, the Brown Limestone (early Campanian) and Sudr Chalk (late Campanian to Maastrichtian...
Journal Article
Published: 01 June 1995
Bulletin of Canadian Petroleum Geology (1995) 43 (2): 156–176.
...- lain unconformably by the Sudr Formation. The unit is very rich in organic matter. It is considered as a potential source rock in the Gulf of Suez (Salah, 1992). Sudr Formation (Maastrichtian ) The Sudr Formation, called the Sudr Chalk by most of the operating oil companies in the Gulf of Suez...
Journal Article
Published: 25 November 2013
Journal of the Geological Society (2014) 171 (2): 239–254.
... or not. The Coniacian–Santonian rocks of the area (Themed Formation; Ziko et al . 1993 ) are 85–105 m thick and are made up of chalky limestone and marl. The Campanian–Maastrichtian rocks are made up of snow-white chalk (Sudr Chalk; Ghorab 1961 ) that is 160–200 m thick. At G. Araif El Naqa ( Fig. 3 ), a clastic...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2000
GeoArabia (2000) 5 (3): 405–424.
... Maastrichtian units of the St. Anthony Formation are composed of siliciclastic carbonates. They correlate with major areas of non-deposition to the north (Northern Galala/Wadi Araba Uplift) and open marine chalk-calcareous shale intercalations of the Sudr Formation farther south in the Southern Galala Sub-basin...
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Journal Article
Published: 01 May 2016
Jour. Geol. Soc. India (2016) 87 (5): 610–622.
... distributed and preserved. The sedimentary successions are from base to top are as follows: Sudr, Dakhla, Tarawan, and Esna formations. The Cretaceous-Paleogene succession in the eastern desert of Egypt have drawn the attention of Several workers (e.g. Hume, 1911 ; Awad and Abdallah, 1966 ; Abdel Kireem...
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Journal Article
Journal: AAPG Bulletin
Published: 11 October 1997
AAPG Bulletin (1997) 81 (10): 1640–1659.
... points and the relationship between the R o (vitrinite reflectance) value and the depth to the oil generation threshold of the source rocks ( Figure 10 ), we can identify the hydrocarbon source kitchens. Three regional structure maps for the potential sources—upper Senonian Sudr Chalk, lower Miocene...
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Journal Article
Published: 07 December 2016
Journal of the Geological Society (2017) 174 (2): 336–352.
... of Wadi Beida and seem to define a stratigraphic interval (though discontinuous) within the Sudr Chalk ( Fig. 9 ). Luning et al. (1998 ) interpreted these sands to have been reworked from the Lower Cretaceous rocks exposed in the core of the anticline. These clastic sediments were transported northward...
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Journal Article
Journal: The Leading Edge
Published: 01 September 2024
The Leading Edge (2024) 43 (9): 578–587.
... unconformity is clear between folded Upper Cretaceous (Turonian and Coniacian) rocks and nearly horizontal Campanian-Maastrichtian chalk and Eocene limestone of Sudr El Heitan Plateau ( Moustafa and Khalil, 1990 ) (see Figure 22b in Moustafa, 2020 ). This area shows clear evidence for Santonian-age folding...
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Journal Article
Published: 01 September 2000
Geological Magazine (2000) 137 (5): 583–591.
...LIONEL CAVIN; NATHALIE BARDET; HENRI CAPPETTA; EMMANUEL GHEERBRANT; SIDI MOHAMED IAROCHENE; JEAN SUDRE Abstract A new albulid fish, Phosphonatator oxyrhynchus , based on a single large neurocranium, is described from the deposits of the Ouled Abdoun phosphatic basin, Morocco. The matrix...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 2003
AAPG Bulletin (2003) 87 (1): 143–180.
... been identified on the basis of total organic carbon (TOC) content and pyrolysis result (S 2 ) within the Gulf of Suez. In stratigraphic ascending order these are the Upper Cretaceous carbonates (Brown Limestone and Sudr Chalk); the Eocene Thebes, lower Miocene Rudeis, and middle Miocene Kareem...
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Journal Article
Published: 04 May 2010
Geological Magazine (2010) 147 (6): 860–870.
..., the oldest evidence of Afrotheria (Gheerbrant, Sudre & Cappetta, 1996 ; Gheerbrant, 2009 ). The species Xiphodolamia serrata (GTS.2, Fig. 3 b), recently described from Priabonian deposits of Jordan, Iran and Angola (Adnet et al . 2009 ), is probably one of the most important elements...
Journal Article
Published: 01 October 2007
Journal of Foraminiferal Research (2007) 37 (4): 393–395.
....—“Thirteen species of Bolivinoides taxa as well as twenty-nine of other benthic association have been mainly recorded from the Sudr Chalk, in addition to the basal part of Esna Shale formation. . . The stratigraphic distribution of the foraminiferal assemblages during this sequence has been led...
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 15–40.
...) to designate the Paleocene-lower Eocene shaly succession between the underlying Maastrichtian Chalk (Sudr Formation, Ghorab 1961 ) and the overlying Thebes Limestone. The planktonic foraminifera of the upper Paleocene-lower Eocene interval in different parts of Egypt, including one or more of the above...
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Journal Article
Published: 01 May 1971
Journal of the Geological Society (1971) 127 (3): 247–271.
... (A) Basement. (B) Nubian Sandstone (e) Cenomanian (D) Turonian. CONTENTS (p.) Santonian (F) Campanian-Maastrichtian (Chalk) (o) Esna Shales (i-i) Eocene . . . . (I) Pre-Oligocene variations in thickness (j) Oligocene (K) Miocene . . (L) Concluding Remarks. Structure. (A) The eastern marginal faults (B...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1961
AAPG Bulletin (1961) 45 (2): 198–218.
..., Minia limestone, Thebes formation (or its equivalent the Farafra limestone), Esna shale, chalk, and Dakhla shale (Aschgraue Blätterthone of Zittel). Although there are some lateral variations in these rock units, these formations can be traced with reasonable accuracy throughout the area...
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Series: SEPM Special Publication
Published: 01 January 2010
DOI: 10.2110/sepmsp.094.155
EISBN: 9781565762985
..., Portland Core, Colorado; K, Niobrara Chalk localities, Kansas; Texas proposed GSSP; E, Western Sinai, Egypt. Map modified from Scotese (1998) . MS Measurements Previous Work Applications and Interpretations of Bulk (Initial) Low-Field Magnetic Susceptibility Fig. 2. —MS data from...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1966
AAPG Bulletin (1966) 50 (7): 1455–1477.
.... In Kharga Oasis, Ball (1900) retained the term “Esna shales” for the series of unfossiliferous, laminated gray clay, shale, and marl which overlie the Upper Cretaceous white chalk and extend to the base of the Eocene limestone. He stated that these sediments “… appear to be a continuation of similar beds...
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