Sökning: "shallow marine environment"

Visar resultat 16 - 20 av 20 uppsatser innehållade orden shallow marine environment.

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

    Magister-uppsats, Lunds universitet/Geologiska institutionen

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

    Sammanfattning : 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. LÄS MER

  3. 17. Lower Ordovician conodonts from Köpings klint, central Öland, and the feeding apparatuses of Oistodus lanceolatus Pander and Acodus deltatus Lindström

    Magister-uppsats, Lunds universitet/Geologiska institutionen

    Författare :Jonas B. Ahnesjö; [1998]
    Nyckelord :Conodonts; Lower Ordovician; Tremadoc; Arenig; biostratigraphy; Öland; Sweden; feeding apparatus; Acodus deltatus; Oistodus lanceolatus; provincialism; facies indicators; Earth and Environmental Sciences;

    Sammanfattning : Köpings klint is located on Öland, SE Sweden and expose a sequence of Lower Ordovician rocks from the boundary between the Tremadoc and the Arenig. The strata are correlated with the Paltodus deltifer, the Paroistodus proteus and the Oepikodus evae conodont Zones. LÄS MER

  4. 18. A conceptual model about nutrients flow in Haapsalu bay

    Master-uppsats, KTH/Industriell ekologi

    Författare :Dolores Soriano Falco; [1998]
    Nyckelord :;

    Sammanfattning : Haapsalu Bay is a very shallow area consisting of semiclosed regions partly separated by peninsulas in the coastal zone of West Estonia. The main inflow of fresh water, 33.875.436 m3/year, from some small rivers (Ungru, Taebla, Vönnu, Asukula) falls into the eastern part of Haapsalu Bay, with the Nitrogen load 72. LÄS MER

  5. 19. Petrology and depositional history of the Campanian strata at Maltesholm, Scania, southern Sweden

    Magister-uppsats, Lunds universitet/Geologiska institutionen

    Författare :Olof Sandström; [1994]
    Nyckelord :Kristianstad basin; Maltesholm; Campanian; grainstone; facies; storm sediments; hummocky cross bedding; conglomerates; shallow marine environment; rudists; belemnites; Earth and Environmental Sciences;

    Sammanfattning : Campanian sediments of the Maltesholm quarry consist of mostly coarse grained, poorly consolidated, ruditic grainstones, almost free of micrite and lime mud, with interbedded clay horizons. The main constituents of the grainstones are coralline algae and quartz. LÄS MER

  7. 20. Agglutinated foraminifera from the Campanian of the Kristianstad basin, southern Sweden

    Kandidat-uppsats, Lunds universitet/Geologiska institutionen

    Författare :Gina Christodoulou; [1993]
    Nyckelord :Kristianstad basin; Maltesholm; Ullstorp; Campanian; biocalcarenite; foraminifera; shallow marine environment; Earth and Environmental Sciences;

    Sammanfattning : In samples consisting mainly of Campanian biocalcarenite from Maltesholm and Ullstorp 23 foraminifera species were identified. The number of species lies within the range for a normal marine environment according to Fisher α-diagrams and triangular diagrams. LÄS MER