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Organisk geokjemi og foraminiferfauna i midtre til øvre jura på Haltenbanken, med vekt på avsetningsmiljøet 
Grønseth, Ole Tom (Master thesis / Hovedoppgave, 2004)
I dette hovedfagsarbeidet gir en stratigrafisk oversikt og faciestolkning av Melke- og Spekkformasjonen fra brønn 6507/7-5, basert på foraminiferanalyser kombinert med data fra organisk geokjemi, for å belyse avsetningsmiljøet ...
Foraminiferstratigrafi og facies av Knorringfjellformasjonen på Svalbard 
Berge, Sigrid Hägg (Master thesis / Hovedoppgave, 2004)
Store deler av Svalbard var i tidsrommet sen trias mellom jura en grunn shelf med kondensert sedimentasjon. Knorringfjellformasjonen representerer avsetningene fra denne perioden i sentrale deler av Spitsbergen. Vekslende ...
Ekofisk Tight Sone: biostratigrafisk analyse og paleomiljøtolkning basert på dinoflagellatcyster 
Haugsmark, Liv Katerine (Master thesis / Hovedoppgave, 2004)
Abstract This thesis is written as a part of the Cand. Scient. degree at the Institute for Geosciences at the University of Oslo. Traditionally, age determinations of late Cretaceous chalks in the Central Graben in the ...
Depositional Environment, Processes and Sequence Stratigraphy of the Paralic Helvetiafjellet Formation in Ullaberget, Southern Spitsbergen 
Ahokas, Juha Matti (Master thesis / Masteroppgave, 2004)
The Early Cretaceous, Barremian – Aptian Helvetiafjellet Formation is a well exposed paralic succession deposited at ramp-type shelf of the Borealic sea in the Svalbard region. The Ullaberget section in the Van Keulenfjorden ...
Deglasiasjon av Van Keulenfjorden, Svalbard, de siste 130 år : Brefrontvariasjoner og glasiale prosesser 
Carlsen, Marit (Master thesis / Hovedoppgave, 2004)
Fronten av fire tidevannsbreer utgjør kalvingsbukta innerst i Van Keulenfjorden, en 43 km lang nordvest-sydøst orientert fjord sydvest på Spitsbergen. Zawadskibreen, Nathorstbreen, Liestølbreen og Doktorbreen går sammen ...
Spor etter Mjølnirnedslaget i Janusfjellprofilet på Svalbard 
Salvigsen, Ottar (Master thesis / Hovedoppgave, 2004)
The 40 km diameter Mjølnir Crater was formed 142 ± 2.6 Ma (Volgian-Ryazanian boundary) by the impact of a 1.6 km diameter asteroid into the 350-400 m deep paleo-Barents Sea. The structure is buried and well preserved in ...
Parameters of the Norwegian Q-system and geological conditions correlated with grout take in the JA1 Skaugum railroad tunnel 
Morgan, Elin Katrine (Master thesis / Hovedoppgave, 2004)
Since its development in 1974 the Q-system for classifying rock masses has readily been used for dimensioning support measures in underground excavations in Norway and internationally. The Q-system, as it was originally ...
The tectonometamorphic development of the Ardencaple Fjord area, North East Greenland Caledonides 
Aas, Tor Even (Master thesis / Hovedoppgave, 2004)
The Caledonian Orogen in East Greenland comprises an autochthonous basement complex overlain by a Late Proterozoic to Early Proterozoic cover sequence with a regionally extensive thrust sheet complex on top. The thrust ...
Inventory Review 2004. Emission data reported to CLRTAP and under the NEC Directive. 
Vestreng, Vigdis; Goodwin, Justin; Adams, Martin (Research report / Forskningsrapport, 2004)
Plesiosaurs from Svalbard 
Andreassen, Bård (Master thesis / Hovedoppgave, 2004)
A re-description and a re-classification is made for the plesiosaur specimen PMO A 27745 previously identified in 1962 as Tricleidus svalbardensis Persson. In all probability the fossil is from the Slottsmøya Member of ...
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Date Issued
2004 (16)
Document TypeHovedoppgave (13)Masteroppgave (2)Forskningsrapport (1)AuthorAas, Tor Even (1)Adams, Martin (1)Ahokas, Juha Matti (1)Akre, Guri Alberte (1)Andreassen, Bård (1)... View More
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