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Tarawan Chalk

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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 139-146.
...Dennis V. Kent; Christian Dupuis Abstract A paleomagnetic study of the Paleocene-Eocene Esna Shale and Tarawan Chalk at the Dababiya and Qreiya sections near Luxor in central Egypt reveals stable normal and reverse polarity magnetizations. However, these (neritic) pelagic marine sediments have...
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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...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 61-92.
.../Eocene boundary. The measured (composite) section extends from the Tarawan Chalk (Zone P4), through the Esna Shale (Zone P4c, P5-8) to the basal Thebes Limestone (Zone P8). Midway-type benthic foraminiferal faunas extend throughout the section and suggest deposition at mid-outer neritic depths...
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Paleomagnetic directions from <b>Tarawan</b> <b>Chalk</b> and Esna Shale.
Published: 01 June 2003
TABLE 1 Paleomagnetic directions from Tarawan Chalk and Esna Shale.
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 179-212.
... correlations of upper Paleocene-lower Eocene sections in the southern Nile Valley are correlated based on the most prominent events. The biostratigraphy of the Tarawan Chalk and Esna Shale are correlated with the Integrated Magnetobiostratigraphic scale of Berggren et al. (1995) . The vertical (stratigraphic...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 41-59.
... comprises the Tarawan Chalk, the Esna Shale and the Thebes Limestone. The horizon that constitutes the P/E GSSP is located in the lower part of the Esna Shale Formation. This formation, remarkably thick (~130m) at Dababiya, is largely of homogenous gray shales. Its lower part includes, however, a thin...
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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...
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Generalized biostratigraphy and characteristic biovents of the <b>Tarawan</b> Chal...
Published: 01 June 2003
TEXT-FIGURE 2 Generalized biostratigraphy and characteristic biovents of the Tarawan Chalk-Esna Shale sequence at G. Qreiya. LO: Lowest Occurrence; HO: Highest Occurrence, LCO: Lowest Common Occurrence; HCO: Highest Common Occurrence, P: Planktonic foraminiferal biozone, NP: Nannoplankton
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Generalized biostratigraphy and characteristic biovents of the <b>Tarawan</b> Chal...
Published: 01 June 2003
TEXT-FIGURE 2 Generalized biostratigraphy and characteristic biovents of the Tarawan Chalk-Esna Shale sequence at G. Qreiya. LO: Lowest Occurrence; HO: Highest Occurrence, LCO: Lowest Common Occurrence; HCO: Highest Common Occurrence, P: Planktonic foraminiferal biozone, NP: Nannoplankton
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Paleopole corresponding to the mean B component direction for the <b>Tarawan</b> C...
Published: 01 June 2003
TEXT-FIGURE 6 Paleopole corresponding to the mean B component direction for the Tarawan Chalk and Esna Shale (star; Table 1 ) compared to reference mean paleopoles for Africa: Ku - Upper Cretaceous; Te-Eocene; To-Oligocene; Tm- Miocene; Tp - Pliocene (compilation of mainly igneous results
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Vector end point diagrams of thermal demagnetization of NRM of representati...
Published: 01 June 2003
TEXT-FIGURE 2 Vector end point diagrams of thermal demagnetization of NRM of representative samples of Tarawan Chalk and Esna Shale. Open/closed symbols projected on vertical/horizontal planes in geographic coordinates. Thermal demagnetization steps labeled in (e). Dababiya section: a) Tarawan
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IRM acquisition (open symbols) and thermal demagnetization (closed symbols)...
Published: 01 June 2003
TEXT-FIGURE 3 IRM acquisition (open symbols) and thermal demagnetization (closed symbols) of representative samples of a) Esna Shale and b) Tarawan Chalk.
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(a) Stratigraphic units exposed in the study area and their distribution in...
in > GeoArabia
Published: 01 January 2003
Figure 5: (a) Stratigraphic units exposed in the study area and their distribution in a N-S profile; (b) Schematic diagram (not to scale) showing the southward thickening of the Khoman Formation, Tarawan Chalk, and Esna Shale away from the Bahariya Depression.
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B component directions obtained from thermal demagnetization of samples fro...
Published: 01 June 2003
TEXT-FIGURE 5 B component directions obtained from thermal demagnetization of samples from Tarawan Chalk and Esna Shale at Dababiya and Qreiya. Open/closed symbols on upper/lower hemisphere of equal-area projection in geographic coordinates.
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Stratigraphical succession on the West Bank. We show here the location of s...
Published: 28 September 2016
of unit 4. However, tombs (e.g. TT28, TT192) were excavated in the Tarawan Chalk at the toe of the block (see location of tombs in Fig. 3 ). P, Paleocene; E, Eocene.
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Magnetic susceptibility and B component inclination as a function of strati...
Published: 01 June 2003
of the Tarawan Chalk with the Esna Shale, which extends to its contact with the Thebes Limestone at the 54m-level in Qreiya and 129m-level at Dababiya.
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Correlation of the main lithologic units of the Paleocene-lower Eocene sequ...
Published: 01 June 2003
Shale Member of Abdel Razik 1972) to the top of the Thebes Limestone as originally defined by Said (1960) . The thickness of the Paleocene Dakhla Shale at Dababiya is estimated by correlation with adjacent areas. B Rock units from the base of the Tarawan Chalk (0.0) to the top of the Esna Shale
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1972
AAPG Bulletin (1972) 56 (8): 1448-1463.
...   Thebes Formation—Limestone with flint containing OpercuyiDa Wbyca Zitt. + 155 YPRESIAN-LANUENIAN   Esna Shale—Shale with thin hmestone bands 34-140 DANIAN   Tarawan ChalkChalk and chalky limestone with dwarfed fauna at top and Ananchytes fakhreyi Fourteau zone at base (this zone recorded...
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Journal Article
Published: 28 September 2016
Proceedings of the Yorkshire Geological Society (2016) 61 (2): 134-147.
... of unit 4. However, tombs (e.g. TT28, TT192) were excavated in the Tarawan Chalk at the toe of the block (see location of tombs in Fig. 3 ). P, Paleocene; E, Eocene. ...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 15-40.
... ; Tantawy et al. 2000 ). The upper part of the Dakhla Formation of Said (1961) , euqivalent to the Lower Owaina Shale Member of El Naggar (1966) : 35m thick; The Tarawan Formation of Awad and Ghobrial (1965) , equivalent to the Middle Owaina Chalk Member of El Naggar (1966) : 17–21m thick...
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