1-19 OF 19 RESULTS FOR

Gebel Owaina Egypt

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 147–166.
...Khaled Ouda; William A. Berggren; Khaled Saad Abstract We describe the planktonic foraminiferal biostratigraphy of the ~61m thick stratigraphic section spanning the Tarawan Chalk (~17 m) and Esna Shale (~44 m) at Gebel Owaina and the ~35m thick section spanning the total thickness of the Esna Shale...
FIGURES | View All (8)
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 105–122.
...William A. Berggren; Khaled Ouda Abstract We describe the upper Paleocene-lower Eocene planktonic foraminiferal biostratigraphy at Qreiya (southeastern exposure of Gebel Abu Had), about 50km ENE of Qena, Egypt. The ~54m thick section spans the Tarawan Chalk (~8.6m thick; Zone P4a+b) and the Esna...
FIGURES | View All (9)
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 93–104.
... order, the LO of Ac. esnaensis and Ig. broedermanni (sample Qc14.4), the LO of Ac. angulosa (sample Qc15) and the LO of Ac. wilcoxensis (sample Qc15.4). A similar sequential distribution pattern has been observed at Dababiya (Ouda and Berggren 2003, chapter 4, this volume) and Owaina (Ouda et al...
FIGURES | View All (6)
Journal Article
Published: 01 January 2007
Micropaleontology (2007) 53 (1-2): 127–144.
... prinsii Zone. This section is regarded as one of the most complete Cretaceous/Paleocene boundary interval in Egypt ( Faris and Abu Shama 2003 ). The Paleocene biozones at Gebel El Mishiti and their characteristics are discussed below: This zone includes the interval from the increased frequency...
FIGURES | View All (9)
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1966
AAPG Bulletin (1966) 50 (7): 1455–1477.
... by the basal formation of the Esna, the Sharawna Shale. This also dips eastward, forming the base of Gebel Owaina, where it is overlain disconformably by the Owaina Shale, the upper formation of the Esna. The Esna Group is widely distributed in Egypt, extending from the Dakhla-Kharga-Kurkur-El-Bargah scarp...
FIGURES | View All (10)
Journal Article
Published: 01 January 2006
Micropaleontology (2006) 52 (3): 193–222.
... . OUDA , KH. , 2003 . The Paleocene/Eocene boundary in Egypt: An overview . Micropaleontology , 49 ( 1 ): 15 – 40 . OUDA , KH. , BERGGREN , W. and SAAD , KH. , 2003 . The Gebel Owaina and Kilabiya sections in the Idfu-Esna area, Upper Nile Valley (Egypt) . Micropaleontology...
FIGURES | View All (18)
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 167–178.
... Valley . Geological Society of Egypt, Thirty third Annual Meeting , Cairo Nov. 18 – 22 , 1995 (Abstract). OUDA , KH. , BERGGREN , W.A. and SAAD , KH. , 2003 . Upper Paleocene-lower Eocene planktonic foraminiferal biostratigraphy of the Gebel Owaina and Kilabiya sections...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1968
AAPG Bulletin (1968) 52 (9): 1792–1793.
... that the division of the Gebel Owaina section into a lower shale unit (the Dakhla Shale), a middle “Chalk” unit, and an upper shale unit (the Esna Shale) is erroneous. El-Naggar went on to state that the Dakhla Shale is a heterogeneous rock unit for it “… includes the Maestrichtian Sharawna Shale, the conglomerate...
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 15–40.
... the 87 Sr/ 86 Sr ratios throughout the Paleocene section at Gebel Owaina and, from the long-term stability of the Sr-isotope record in it, concluded that there were no major changes in tectonic activity, weathering rates or hydrothermal activity during the Paleocene in southern Egypt. The chemical...
FIGURES | View All (13)
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1968
AAPG Bulletin (1968) 52 (9): 1794–1798.
...). In the last reference, it is clearly stated (p. 356) that “… El-Naggar, in his work on the type section of the Esna Shales at Gebel Owaina in Upper Egypt (Ms.) has distinguished three zones in the Paleocene on the basis of the planktonic foraminifera. These zones can also be distinguished in world-wide...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1972
AAPG Bulletin (1972) 56 (8): 1448–1463.
... see El-Naggar, 1966 ), although the regional mapping of the area was done only recently by the Geological Survey of Egypt ( Issawi and Bassiyouni, 1959 ). Said (1962) , Said and Sabry (1964) , and El-Naggar (1966) classified the section in Gebel Owaina, 30 km southeast of Esna, into the units...
FIGURES | View All (6)
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 61–92.
... on the Geological Map of Egypt ( Klitzsch et al. 1981 ) and precisely located on the geological map established for Gebel El Shaghab area by Khalifa (1970) . The planktonic foraminiferal zonation of Berggren et al. (1995=BKSA95) is used here. However, based on the studies of sections in the upper Nile Valley...
FIGURES | View All (17)
Journal Article
Published: 01 March 2013
Journal of the Geological Society (2013) 170 (2): 341–352.
... a precision better than 5%. In addition, P tot analyses were performed on several other sections from the central Eastern Desert of Egypt (e.g. Gebel Duwi, Bolle et al . (2000) ; Dababiya Global Stratotype Section and Point (GSSP), Dupuis et al . 2003 ) and from central Sinai (Abu Zenima and Gebel...
FIGURES | View All (9)
Journal Article
Published: 28 September 2016
Proceedings of the Yorkshire Geological Society (2016) 61 (2): 134–147.
... narrow and shallow graben of the Valley of the Kings, with an offset of c. 30 m ( Curtis 1979 ). The three geological formations of the subtabular bedrock of the West Bank ( Fig. 3 ) are widespread in Upper Egypt and can be seen in gebels along the Nile Valley, from Qena in the north to south...
FIGURES | View All (12)
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 179–212.
... the Working Group examined numerous sections in Egypt, finally focusing on the following (from north to south): 1) Gebel Qreiya (southeastern exposure of Gebel Abu Had), 2) Dababiya, 3) Gebel Owaina, 4) Gebel Kilabiya, and 5) Wadi Abu Ghurra (text-fig. 1 ). A primary focus of these studies has been...
FIGURES | View All (18)
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): ii–iv.
.... Although difficult of access, sections such as Gebel Owaina have long been the reference for the lower Paleogene of Egypt. The search for a P/E GSSP has prompted the reinvestigation of these classic sections together with the study of new sections such as Dababiya, in an effort to find land sections...
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 41–59.
... spectacular lower Paleogene successions form a succession of high cliffs (or gebels) that dominate the Nile Valley. Whereas several upper Paleocene-lower Eocene sections, as for instance the Gebel Owaina section, have become well known to geologists, the remarkable exposures in the vast quarry at Dababiya...
FIGURES | View All (9)
Image
figs 1–3 .  Acarinina sibaiyaensis (El-Naggar) 1966, holotype:  1 , umbilic...
Published: 01 May 2008
, side view; 6 , spiral view. Collection number P.45593, the NHM. (figs 1–6 all from sampleS. 50, 8 m above the base of the Esna Formation (‘upper Owaina Shale’) at Gebel Aweina (‘Owaina’), Nile Valley, Egypt.) figs 7–11 . Acarinina multicctmerata n. sp., holo type: 7 , umbilical view; 8 , side
Journal Article
Published: 01 May 2008
Journal of Micropalaeontology (2008) 27 (1): 5–12.
... , side view; 6 , spiral view. Collection number P.45593, the NHM. (figs 1–6 all from sampleS. 50, 8 m above the base of the Esna Formation (‘upper Owaina Shale’) at Gebel Aweina (‘Owaina’), Nile Valley, Egypt.) figs 7–11 . Acarinina multicctmerata n. sp., holo type: 7 , umbilical view; 8 , side...
FIGURES | View All (4)