• Upper Paleocene-lower Eocene calcareous nannofossil

    Dababiya Quarry Beds (DQBs Dupuis et al. 2003) that were documented in several sections in Egypt (Tantawy 2006 Khozyem et al. 2013). 2. Studied section and methods Twenty-two bulk rock samples were investigated from the upper Paleocene-lower Eocene at the Misheiti Section Central Sinai Egypt (Figure 1). Smear slides were prepared

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  • Nature of the Paleocene/Eocene (P/E) boundary in Sinai

    2017-12-1 · The Dababiya Quarry Section Lithostratigraphy clay mineralogy geochemistry and paleontology Kh Ouda M.-P. Aubry (Eds.) The Upper Paleocene-Lower Eocene of the Upper Nile Valley Stratigraphy Micropaleontology vol. 49(1) ( 2003 ) pp. 4159

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  • (PDF) The Dababiya Core A window into Paleocene to Early

    The composite Paleocene-lower Eocene Dababiya section recovered in the Dababiya Quarry core and accessible in out-crop in the Dababiya Quarry exhibits an unexpected contrast in thickness between the Lower Eocene succession ( Esna Shales) and the

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  • Fluvial discharge and sea-level changes controlling black

    2017-5-30 · focuses on the Dababiya Quarry section which is located near the Forada Dababiya Bighorn Leg 208 Site 1051 Site 690 55.0 Ma reconstruction Shelf sites Continental sites Deep marine sites Leg 302 Southern Ocean Tethys Pacific Ocean Atlantic Ocean Fig. 1. Paleogeographic location of the Dababiya Quarry section and other important PETM sites.

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  • Calcareous nannofossils of the Paleocene–Eocene

    the Global Stratotype Section and Point (GSSP) at the base of the Eocene in the Dababiya Quarry Luxor Egypt. The P/E boundary is placed at the base of the Carbon Isotope Excursion (CIE) in the Dababiya Quarry section (Aubry and Ouda 2003). The primary goals of the present study were to 1) document a high-resolution biostratigraphic

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  • Upper Paleocene-lower Eocene calcareous nannofossil

    Dababiya Quarry Beds (DQBs Dupuis et al. 2003) that were documented in several sections in Egypt (Tantawy 2006 Khozyem et al. 2013). 2. Studied section and methods Twenty-two bulk rock samples were investigated from the upper Paleocene-lower Eocene at the Misheiti Section Central Sinai Egypt (Figure 1). Smear slides were prepared

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  • The Dababiya Quarry (southeast Luxor Egypt) a unique

    2021-2-20 · The Dababiya Quarry for example is a unique palaeogeographical geosite located in the south Eastern Desert of Egypt about 35 km southeast of the historical Pharaonic city of Luxor. The quarry is made up of sedimentary successions of Late Cretaceous–Quaternary age (Aubry et al. 2007).

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  • Geochemistry The Dababiya Quarry Section

    Dababiya Quarry El Mahmiya and Abu Had members. In the present study the Esna Formation was sampled and described. The total thickness is about 17.5 m at the Gabal Umm El Ghanayim section and about 10 m at the Naqb Assiut section. This rock unit represents the El-Hanadi El Dababiya Quarry and the lower part of El­Mahmiya Member (Figs. 2 and

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  • The Dababiya Quarry Section Lithostratigraphy Clay

    Christian Dupuis et al. The Dababiya Quarry Section Lithostratigraphy clay mineralogy geochemistry and paleontology DBD m 120 110_ cc 1UU_ 0e cn i 90_ O 80 G) 470_ 0 60_ a) 20_ DBH 10_--9 DBA Key beds pk3 DBD THEBES 113 108.5 99.5 92 ESNA 3 79.5 69.5 61-62 37-38 ESNA 2 3 7 /b Dababiya Quarry Beds ESNA 1 DBAO TARAWAN DB comp. lom DAKHLA

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  • Geological heritage of Luxor and its vicinities Egypt a

    2020-1-11 · Geological heritage is an important resource for socio-economic development of Egypt and thus it requires careful exploration. Potentially unique geological features available in Luxor city and its vicinities including the Dababiya Protectorate are reassessed on the basis of literature review and field work. This permits to establish six geological heritage types namely stratigraphical

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  • DababiyaUNESCO World Heritage Centre

    The GSSP is defined in the huge Quarry of Dababiya located on the eastern bank of the Nile Valley 35 km South of Luxor. The Dababiya Quarry Beds 3.5 m thick in the stratotypic section and consisting of 5 distinctive units constitute a remarkable record of the Carbon Isotope Excursion (CIE) and the P/E Thermal Maximum (PETM) whose causes are

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  • The Dababiya Quarry (southeast Luxor Egypt) a unique

    2021-2-20 · The Dababiya Quarry for example is a unique palaeogeographical geosite located in the south Eastern Desert of Egypt about 35 km southeast of the historical Pharaonic city of Luxor. The quarry is made up of sedimentary successions of Late Cretaceous–Quaternary age (Aubry et al. 2007).

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  • The Dababiya Quarry section Lithostratigraphy clay

    The Global Standard Stratotype-section (GSSP) for the Paleocene/Eocene (P/E) boundary has been selected in the Dababiya Quarry near Luxor at the base of a lithostratigraphic unit where the base of the so-called Carbon Isotope Excursion (CIE) is recorded.

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  • The Global Standard Stratotype-section and Point (GSSP

    The GSSP for the base of the Eocene Series is located at 1.58 m above the base of Section DBH in the Dababiya Quarry on the east bank of the Nile River about 35 km south of Luxor Egypt. It is the base of Bed 1 of the Dababyia Quarry Beds of the El Mahmiya Member of the Esna Formation interpreted as having recorded the basal inflection of

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  • Nature of the Paleocene/Eocene (P/E) boundary in Sinai

    2017-12-1 · The Dababiya Quarry Section Lithostratigraphy clay mineralogy geochemistry and paleontology Kh Ouda M.-P. Aubry (Eds.) The Upper Paleocene-Lower Eocene of the Upper Nile Valley Stratigraphy Micropaleontology vol. 49(1) ( 2003 ) pp. 4159

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  • ‪Marie-Pierre Aubry‬‪Google Scholar‬

    The Dababiya Quarry Section Lithostratigraphy clay mineralogy geochemistry and paleontology C Dupuis MP Aubry E Steurbaut WA Berggren K Ouda R Magioncalda Micropaleontology 49 (Suppl_1) 41-59 2003

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  • The Qreiya Section at Gebel Abu Had Lithostratigraphy

    2003-6-1 · A detailed study of the Dababiya Quarry Beds has revealed distinct stratigraphic trends in both mineralogy and geochemistry similar to those reported from Dababiya Quarry itself. In particular the organic carbon isotope analysis has revealed a pronounced negative carbon isotope excursion of comparable magnitude to that recorded from Dababiya.

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  • The Dababiya Core Awindow into Paleocene to Early

    2013-7-26 · The Dababiya Quarry Core (DBQc) provided significant in-sights into the geological history of Upper Egypt as discussed in contributions in this volume. An unanticipated discovery was the striking contrast between the thinness ( 70 m) of the Paleocene section in

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  • Biostratigraphy and depositional environments of the

    2020-11-24 · Moreover the Esna Shale is further subdivided into four members arranged from base to top as El Hanadi Dababiya Quarry El Mahmiya and Abu Had. The depositional setting is interpreted to primarily reflect the relative sea‐level changes.

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  • (PDF) The Dababiya corehole Upper Nile Valley Egypt

    The Dababiya corehole Upper Nile Valley Egypt preliminary results. 2012. Christian Dupuis

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  • DababiyaUNESCO World Heritage Centre

    The Dababiya Quarry Beds 3.5 m thick in the stratotypic section and consisting of 5 distinctive units constitute a remarkable record of the Carbon Isotope Excursion (CIE) and the P/E Thermal Maximum (PETM) whose causes are still being actively debated. Indeed the base of the CIE allows global (i.e. marine-terrestrial) correlations of the

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  • (PDF) The Dababiya Quarry Section Lithostratigraphy clay

    The Global Standard Stratotype-section (GSSP) for the Paleocene/Eocene (P/E) boundary has been selected in the Dababiya Quarry near Luxor at the base of a lithostratigraphic unit where the base

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  • Limestone Rock Quarry Operation Lci

    Geochemistry The Dababiya Quarry Section. Limestone Rock Quarry Operation Lci Panola. Limestone Rock Quarry Operation Lci. 33 lci boundaries 331 limestone quarry operations the lci for quarry operations includes the inputs and outputs for each of the processes depicted in figure 1 specifically processes and operations represented in the

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  • (PDF) The Dababiya Core A window into Paleocene to Early

    The composite Paleocene-lower Eocene Dababiya section recovered in the Dababiya Quarry core and accessible in out-crop in the Dababiya Quarry exhibits an unexpected contrast in thickness between the Lower Eocene succession ( Esna Shales) and the

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  • Palaeoenvironmental turnover across the Palaeocene/Eocene

    2005-8-15 · The Global Stratotype Section and Point for the Palaeocene/Eocene (P/E) boundary was defined at Dababiya Quarry (Egypt) at the base of the carbon

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  • The Dababiya Core Awindow into Paleocene to Early

    2013-7-26 · The Dababiya Quarry Core (DBQc) provided significant in-sights into the geological history of Upper Egypt as discussed in contributions in this volume. An unanticipated discovery was the striking contrast between the thinness ( 70 m) of the Paleocene section in

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  • (Prof. Khaled Abdel-Kader Ouda)Assiut University

    2015-6-3 · In the ballot the members of the WG voted unanimously in favor of placing the GSSP for the base of the Eocene Series in the DBH partial section located in the abandoned quarry of Dababiya eastern side of the Upper Nile Valley about 35 km south of Luxor Egypt.

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