Essays about: "depositional environments"

Showing result 16 - 20 of 22 essays containing the words depositional environments.

  1. 16. Sedimentary facies and fauna of the Late Silurian Bjärsjölagård Limestone Member (Klinta Formation), Skåne, Sweden

    University essay from Lunds universitet/Geologiska institutionen

    Author : Susanne Nilsson; [2006]
    Keywords : Bjärsjölagårdkalkstenen; Ludlow; sedimentära facies; faunadiversitet; Laukatastrofen; stratigrafisk korrelation; Skåne; The Bjärsjölagård Limestone Member; sedimentary facies; faunal diversity; Lau Event; stratigraphical correlation; Earth and Environmental Sciences;

    Abstract : Bjärsjölagårdkalkstenen i Skåne, södra Sverige, är av sen ludlowålder och utgör en del av Klintaformationen inom Öved-Ramsåsagruppen. Denna kalksten bildades under tiden för den globalt kända Laukatastrofen och ett kraftigt havsnivåfall i den Baltiska bassängen. READ MORE

  2. 17. Correlation between diagenesis and sedimentary facies of the Bentheim Sandstone, the Schoonebeek field, The Netherlands

    University essay from Lunds universitet/Geologiska institutionen

    Author : Pär Malmborg; [2002]
    Keywords : Bentheim Sandstone; sedimentary facies; diagenesis; petroleum reservoir; Lower Cretaceous; Valanginian; Lower Saxony Basin; Schoonebeek; Gildehaus; Earth and Environmental Sciences;

    Abstract : The Valanginian (Lower Cretaceous) Bentheim succession of the Schoonebeek field is deposited in a shallow-marine environment along the southern and southwestern coast of the Lower Saxony Basin in eastern Netherlands. Three cores from Schoonebeek field, selected by NAM (Nederlandse Aardolie Maatschappij), and a number of samples from an outcrop in the Bentheim Sandstone at Gildehaus were studied. READ MORE

  3. 18. Reconstruction of fan-shaped outwash in front of the Mýrdalsjökull ice cap, Iceland : architecture and style of sedimentation

    University essay from Lunds universitet/Geologiska institutionen

    Author : Lina Sultan; [2002]
    Keywords : alluvial fans; Hochsanders; sediment architecture; supraglacial material; tephra; lceland; Earth and Environmental Sciences;

    Abstract : Populärvetenskaplig sammanfattning: Smältvatten som transporteras från en glaciär för med sig material som kan ansamlas framför iskanten. De landformer som då bildas får olika karaktär beroende på t.ex. hur materialet transporteras dit och hur depositionen går till. READ MORE

  4. 19. Trace fossils from the Permian of western Dronning Maud Land, Antarctica

    University essay from Lunds universitet/Geologiska institutionen

    Author : Jenny Sälgeback; [1999]
    Keywords : trace fossils; Permian; Antarctica; non-marine; Scoyenia ichnofacies; Aulichnites; Cochlichnus; Helminthopsis; Lockeia; Palaeophycus; Skolithos; Earth and Environmental Sciences;

    Abstract : Non-marine trace fossils from the Permian of Antarctica are systematically described and possible depositional environments are discussed. The studied material derives from sedimentary sequences consisting mainly of sandstone and shale at Vestfjella and Kirwanveggen, western Dronning Maud Land. READ MORE

  5. 20. The Brennvinsfjorden Group of southern Botniahalvøya, Nordaustlandet, Svalbard : structure, stratigraphy and depositional environment

    University essay from Lunds universitet/Geologiska institutionen

    Author : Johan Nilsson; [1997]
    Keywords : The Brennvinsfjorden Group; the Goosbukta Anticline; the Gottwaldhøgda Fault; the Kapp Hansteen Group; Botniahalvøya; Nordaustlandet; Svalbard; Earth and Environmental Sciences;

    Abstract : Populärvetenskaplig sammanfattning: Den sedimentära enheten Brennevinsfjorden Group på Botniahalvøya, nordvästra Nordaustlandet, underlagrar diskordant en vulkanisk enhet av Grenvillisk ålder (Kapp Hansteen Group). De studier av Brennevinsfjorden Group som presenteras i detta arbete påvisar en ny stratigrafi och en bättre geografisk placering och tolkning av strukturen under basalkonglomeratet som utgör gränsen mellan Kapp Hansteen Group och Brennevinsfjorden Group. READ MORE