FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2102906350> ?p ?o ?g. }

• W2102906350 endingPage "104" @default.
• W2102906350 startingPage "93" @default.
• W2102906350 abstract "Research Article| June 01, 2003 The Qreiya Section at Gebel Abu Had: Lithostratigraphy, clay mineralogy, geochemistry and biostratigraphy Robert W. O’B. Knox; Robert W. O’B. Knox 1c/o British Geological Survey, Keyworth, Nottingham NG12 5GG, UK Search for other works by this author on: GSW Google Scholar Marie-Pierre Aubry; Marie-Pierre Aubry 2Department of Geology, Rutgers University, 610 Taylor Road, Piscataway, New Jersey, USA3Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar William A. Berggren; William A. Berggren 2Department of Geology, Rutgers University, 610 Taylor Road, Piscataway, New Jersey, USA3Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar Christian Dupuis; Christian Dupuis 4Faculté Polytechnique de Mons, rue de Houdain 9, B-7000 Mons, Belgium 08554, USA Search for other works by this author on: GSW Google Scholar Khaled Ouda; Khaled Ouda 5Department of Geology, University of Assiut, Assiut, Egypt, email: robertknox@rknox.fsnet.co.uk Search for other works by this author on: GSW Google Scholar Roberto Magioncalda; Roberto Magioncalda 4Faculté Polytechnique de Mons, rue de Houdain 9, B-7000 Mons, Belgium 08554, USA Search for other works by this author on: GSW Google Scholar Mamdouh Soliman Mamdouh Soliman 5Department of Geology, University of Assiut, Assiut, Egypt, email: robertknox@rknox.fsnet.co.uk Search for other works by this author on: GSW Google Scholar Author and Article Information Robert W. O’B. Knox 1c/o British Geological Survey, Keyworth, Nottingham NG12 5GG, UK Marie-Pierre Aubry 2Department of Geology, Rutgers University, 610 Taylor Road, Piscataway, New Jersey, USA3Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA William A. Berggren 2Department of Geology, Rutgers University, 610 Taylor Road, Piscataway, New Jersey, USA3Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Christian Dupuis 4Faculté Polytechnique de Mons, rue de Houdain 9, B-7000 Mons, Belgium 08554, USA Khaled Ouda 5Department of Geology, University of Assiut, Assiut, Egypt, email: robertknox@rknox.fsnet.co.uk Roberto Magioncalda 4Faculté Polytechnique de Mons, rue de Houdain 9, B-7000 Mons, Belgium 08554, USA Mamdouh Soliman 5Department of Geology, University of Assiut, Assiut, Egypt, email: robertknox@rknox.fsnet.co.uk Publisher: Micropaleontology Press First Online: 06 Mar 2017 Online ISSN: 0026-2803 Print ISSN: 1937-2795 © 2003 The Micropaleontology Project, Inc. Micropaleontology (2003) 49 (Suppl_1): 93–104. https://doi.org/10.2113/49.Suppl_1.93 Article history First Online: 06 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Robert W. O’B. Knox, Marie-Pierre Aubry, William A. Berggren, Christian Dupuis, Khaled Ouda, Roberto Magioncalda, Mamdouh Soliman; The Qreiya Section at Gebel Abu Had: Lithostratigraphy, clay mineralogy, geochemistry and biostratigraphy. Micropaleontology 2003;; 49 (Suppl_1): 93–104. doi: https://doi.org/10.2113/49.Suppl_1.93 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyMicropaleontology Search Advanced Search Abstract Calcareous nannofossil and planktonic foramininferal assemblages demonstrate that the succession at Qreiya provides a virtually complete stratigraphic reference section through the Esna Shale Formation.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. Calcareous nannoplankton (Rhomboaster spp.-Discoaster araneus association) and planktonic foraminiferal occurrences (the so-called excursion taxa) allow unambiguous determination of this isotopic excursion as the Carbon Isotope Excursion (CIE) identified globally at the base of Eocene successions.Preliminary petrological analysis of mudstones within the Dababiya Quarry Beds has revealed a finely granular texture, possibly representing fecal pellets. This texture indicates that the sea-bed sediment may have been mobile, and subject to redistribution by gentle, wave-induced currents. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2102906350 created "2016-06-24" @default.
• W2102906350 creator A5009989570 @default.
• W2102906350 creator A5022907790 @default.
• W2102906350 creator A5032002400 @default.
• W2102906350 creator A5054821774 @default.
• W2102906350 creator A5074605029 @default.
• W2102906350 creator A5076599330 @default.
• W2102906350 creator A5077557170 @default.
• W2102906350 date "2003-06-01" @default.
• W2102906350 modified "2023-10-18" @default.
• W2102906350 title "The Qreiya Section at Gebel Abu Had: Lithostratigraphy, clay mineralogy, geochemistry and biostratigraphy" @default.
• W2102906350 cites W1609472728 @default.
• W2102906350 cites W1963974593 @default.
• W2102906350 cites W1964116684 @default.
• W2102906350 cites W1976215537 @default.
• W2102906350 cites W2014921098 @default.
• W2102906350 cites W2025149153 @default.
• W2102906350 cites W2026891921 @default.
• W2102906350 cites W2027582477 @default.
• W2102906350 cites W2032855124 @default.
• W2102906350 cites W2046042118 @default.
• W2102906350 cites W2048332011 @default.
• W2102906350 cites W2068270184 @default.
• W2102906350 cites W2075175542 @default.
• W2102906350 cites W2082540964 @default.
• W2102906350 cites W2090777276 @default.
• W2102906350 cites W2121317826 @default.
• W2102906350 cites W2283276863 @default.
• W2102906350 cites W2319988614 @default.
• W2102906350 cites W2331827382 @default.
• W2102906350 cites W2346193300 @default.
• W2102906350 cites W2525733184 @default.
• W2102906350 cites W2605531097 @default.
• W2102906350 cites W239814605 @default.
• W2102906350 doi "https://doi.org/10.2113/49.suppl_1.93" @default.
• W2102906350 hasPublicationYear "2003" @default.
• W2102906350 type Work @default.
• W2102906350 sameAs 2102906350 @default.
• W2102906350 citedByCount "34" @default.
• W2102906350 countsByYear W21029063502013 @default.
• W2102906350 countsByYear W21029063502014 @default.
• W2102906350 countsByYear W21029063502015 @default.
• W2102906350 countsByYear W21029063502017 @default.
• W2102906350 countsByYear W21029063502018 @default.
• W2102906350 countsByYear W21029063502019 @default.
• W2102906350 countsByYear W21029063502020 @default.
• W2102906350 countsByYear W21029063502021 @default.
• W2102906350 countsByYear W21029063502022 @default.
• W2102906350 countsByYear W21029063502023 @default.
• W2102906350 crossrefType "journal-article" @default.
• W2102906350 hasAuthorship W2102906350A5009989570 @default.
• W2102906350 hasAuthorship W2102906350A5022907790 @default.
• W2102906350 hasAuthorship W2102906350A5032002400 @default.
• W2102906350 hasAuthorship W2102906350A5054821774 @default.
• W2102906350 hasAuthorship W2102906350A5074605029 @default.
• W2102906350 hasAuthorship W2102906350A5076599330 @default.
• W2102906350 hasAuthorship W2102906350A5077557170 @default.
• W2102906350 hasConcept C112698675 @default.
• W2102906350 hasConcept C127313418 @default.
• W2102906350 hasConcept C144133560 @default.
• W2102906350 hasConcept C151730666 @default.
• W2102906350 hasConcept C161191863 @default.
• W2102906350 hasConcept C166957645 @default.
• W2102906350 hasConcept C2780129039 @default.
• W2102906350 hasConcept C2781113848 @default.
• W2102906350 hasConcept C40616122 @default.
• W2102906350 hasConcept C41008148 @default.
• W2102906350 hasConcept C61721801 @default.
• W2102906350 hasConcept C6494504 @default.
• W2102906350 hasConcept C95457728 @default.
• W2102906350 hasConceptScore W2102906350C112698675 @default.
• W2102906350 hasConceptScore W2102906350C127313418 @default.
• W2102906350 hasConceptScore W2102906350C144133560 @default.
• W2102906350 hasConceptScore W2102906350C151730666 @default.
• W2102906350 hasConceptScore W2102906350C161191863 @default.
• W2102906350 hasConceptScore W2102906350C166957645 @default.
• W2102906350 hasConceptScore W2102906350C2780129039 @default.
• W2102906350 hasConceptScore W2102906350C2781113848 @default.
• W2102906350 hasConceptScore W2102906350C40616122 @default.
• W2102906350 hasConceptScore W2102906350C41008148 @default.
• W2102906350 hasConceptScore W2102906350C61721801 @default.
• W2102906350 hasConceptScore W2102906350C6494504 @default.
• W2102906350 hasConceptScore W2102906350C95457728 @default.
• W2102906350 hasIssue "Suppl_1" @default.
• W2102906350 hasLocation W21029063501 @default.
• W2102906350 hasOpenAccess W2102906350 @default.
• W2102906350 hasPrimaryLocation W21029063501 @default.
• W2102906350 hasRelatedWork W1758396658 @default.
• W2102906350 hasRelatedWork W2093776561 @default.
• W2102906350 hasRelatedWork W2350284515 @default.
• W2102906350 hasRelatedWork W2357676215 @default.
• W2102906350 hasRelatedWork W2789304626 @default.
• W2102906350 hasRelatedWork W2789704814 @default.
• W2102906350 hasRelatedWork W2895595942 @default.
• W2102906350 hasRelatedWork W3144680029 @default.
• W2102906350 hasRelatedWork W2740801233 @default.
• W2102906350 hasRelatedWork W3110989845 @default.

• next