1-20 OF 28 RESULTS FOR

Idfu 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.
... of the Gebel Owaina and Gebel Kilabiya sections, Idfu-Esna region. Gebel Owaina (Latitude 25°15′N; Longitude 32°45′E) forms a conspicuous landmark along the eastern side of the upper Nile Valley between Esna and Idfu, about 25km SE of Esna and 8.5km NE of the Sebaia railway station, where it rises about...
FIGURES | View All (8)
Image
—Key map, showing location of Esna-<b>Idfu</b> region, <b>Egypt</b>.
Published: 01 July 1966
Fig. 1. —Key map, showing location of Esna-Idfu region, Egypt.
Image
—Generalized stratigraphic section, Esna-<b>Idfu</b> region, <b>Egypt</b>. Nubia Sandston...
Published: 01 July 1966
Fig. 3. —Generalized stratigraphic section, Esna-Idfu region, Egypt. Nubia Sandstone and Sibaiya (phosphate) Formation belong to Nubia Group (Senonian). Sharawna Shale (Maestrichtian) and Owaina Shale (Paleocene) comprise Esna Group. Thebes Formation (Eocene) is in lower part of Libya Group.
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1966
AAPG Bulletin (1966) 50 (7): 1455–1477.
...Fig. 1. —Key map, showing location of Esna-Idfu region, Egypt. ...
FIGURES | View All (10)
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 1–13.
..., Mineralogical and Sedimentological studies on phosphorites of the Nile Valley (Duwi Formation) between Qena and Idfu, Egypt , Ph.D. Thesis, Technical University , Berlin , 163 pp. + 5Pl . ABD EL-RAZIK , T. M. , and RAZVALIAEV , A. V. , 1972 . On the tectonic origin of the Nile Valley between...
FIGURES | View All (6)
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 167–178.
... . Stratigraphy and planktonic foraminifera of Upper Cretaceous-Lower Tertiary succession in the Esna-Idfu region, Nile Valley, Egypt . Bulletin of the British Museum (Natural History), Geological Supplement 2 : 1 – 291 . HENDRIKS , F. , LUGER , P. , KALLENBACH , H. and SCHROEDER , J.H...
FIGURES
Journal Article
Journal: Economic Geology
Published: 01 March 2008
Economic Geology (2008) 103 (2): 405–424.
... fineness in secondary sites. The Um Egat and Dungash deposits of the Eastern Desert of Egypt are both hosted by Neoproterozoic greenschist facies metavolcanic and metasedimentary rocks that are tectonically overlain by ophiolitic slices emplaced during an arc–back-arc collisional event (e.g., Stern...
FIGURES | View All (19)
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1968
AAPG Bulletin (1968) 52 (9): 1794–1798.
... in the Nile Valley, Egypt : unpub. ms., read before Geol. Soc. Egypt , Cairo , June 26 , 1957 . El-Naggar , Z. R. , 1963 , Geology and stratigraphic paleontology of the Esna-Idfu region, Nile Valley, Egypt, U. A. R. : unpub. Ph.D. thesis, Univ. Wales , U. K . El-Naggar , Z. R...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1972
AAPG Bulletin (1972) 56 (8): 1448–1463.
...Issawi Bahay Abstract The Upper Cretaceous-lower Tertiary sedimentary rocks in central and southern Egypt are characterized by gradual facies differentiation of three main types—Nile Valley, Garra-El Arbain, and Farafra. These facies are present in three different basins within the marginal trough...
FIGURES | View All (6)
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1972
AAPG Bulletin (1972) 56 (5): 882–902.
... colors. In the Nukhul-Baba area, it is generally whitish and pale brown, with abundant crossbedding. Said (1962 , p. 165) stated that there is a wholly clastic Jurassic section, 370 m thick, present in the subsurface of the Baba area. In more recent literature on the Jurassic of Egypt ( Barakat...
FIGURES | View All (12)
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1968
AAPG Bulletin (1968) 52 (4): 601–614.
...Mourad I. Youssef ABSTRACT Most of the structural elements of Egypt could be fitted into a pattern that appears to have been originated by compressive stresses that acted mainly from N. 10° W. and S. 10° E. During the Precambrian these stresses already were active and they produced shears which...
FIGURES
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 15–40.
...Khaled Ouda Abstract The search for a Global Standard Stratotype-section and Point (GSSP) for the Paleocene/Eocene boundary has resulted in several concurrent studies of the Upper Paleocene-Lower Eocene interval in sections across Egypt from the Eastern and Western Deserts to Upper Egypt where...
FIGURES | View All (13)
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1979
AAPG Bulletin (1979) 63 (6): 975–983.
... of the phosphate-bearing Cretaceous and Paleogene sediments of the Nile Valley between Idfu and Qena, in Studies on some mineral deposits of Egypt : Egypt Geol. Survey Art. 7 , p. 109 – 134 . Hilmy , M. E. , et al , 1976 , Sedimentology and paleocurrent study of Nubia Sandstone in Kharga Oasis...
FIGURES | View All (4)
Journal Article
Published: 01 February 2012
Clays and Clay Minerals (2012) 60 (1): 76–88.
... Desert of Egypt, was studied in detail and compared to a fresh, subsurface glauconitic sandstone from the underground mine. Even within this single surface layer, the brownish-green glauconite grains vary in color and chemical composition. From top to bottom, the grains show an increase in Fe and K...
FIGURES | View All (7)
Journal Article
Published: 01 January 2006
Micropaleontology (2006) 52 (3): 193–222.
...Abdel Aziz A. M. Tantawy Abstract The Paleocene-Eocene transition is exposed at Gebel Serai, 50km east of Qena, and at Taramsa, 10km west of Qena in the central Nile Valley of Egypt. The continuous deposition across the P/E boundary, the negative δ 13 C excursion (CIE), the good preservation...
FIGURES | View All (18)
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): 61–92.
... has been paid to the biostratigraphy of this area. This work describes the planktonic foraminiferal biostratigraphy of the upper Paleocene-lower Eocene composite stratigraphic section at Dababiya, ~23km south of Luxor in the upper Nile Valley (Egypt) which includes the recently designated Global...
FIGURES | View All (17)
Journal Article
Published: 01 February 1983
Journal of the Geological Society (1983) 140 (1): 75–95.
...A. C. Ries; R. M. Shackleton; R. H. Graham; W. R. Fitches Abstract A detailed structural traverse across the basement rocks of the Eastern Desert of Egypt shows that they consist, apart from intrusions, of four broadly recumbent tectonic units. The lowest, of arkosic metasediments of continental...
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 February 2010
Lithosphere (2010) 2 (1): 13–32.
...Mohamed Abd El-Wahed; Mahmoud Ashmawy; Hossam Tawfik Abstract We examine the evolution of the northwestern Red Sea, Egypt, by study of the Quseir–Umm Gheig subbasin. The subbasin records two main tectonic events. The first event is related to development of Late Cretaceous synclinal basins due...
FIGURES | View All (13)
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1973
AAPG Bulletin (1973) 57 (4): 741–745.
...Bahay Issawi ABSTRACT A total of 154.7 m of clastic rocks described herein from Bargat El Shab area in southwestern Egypt is considered a type section for the Nubia Sandstone. The section is divided into three members: Shab, Quseir, and Taref. At the type locality a fossiliferous Paleocene...
FIGURES