• Basin analysis and diagenetic investigations of Early and Middle Triassic sediments on Mariaholmen, Svalbard 

      Riise, Henrik Erevik (Master thesis; Mastergradsoppgave, 2016-05-09)
      Subsequent to a widespread hiatus at the top of the Permian on western Svalbard, the Triassic Vardebukta, Tvillingodden and Bravaisberget formations were deposited. In this thesis, the sedimentology, geochemistry and diagenesis are investigated to determine the depositional environment and basinal setting of the Triassic deposits. In the investigated profile on Mariaholmen, only the upper part ...
    • The Bigganjárgga Tillite re-visited: a stratigraphic and sedimentological study 

      Edvardsen, Egil (Master thesis; Mastergradsoppgave, 2019-05-15)
      The Neoproterozoic “tillite”-bearing sequences of the Smalfjord Formation in Varanger, northern Norway have retrieved considerable attention in geological literature since first described and discovered over a century ago. Much of the attention relates to the so-called Reusch’s Moraine also known as the Bigganjárgga Tillite, which rests directly on top of a striated sandstone surface pointing to ...
    • Bretilbaketrekningshistorie og landformer foran Steindalsbreen, Lyngen, Troms 

      Nilsen, Carina (Master thesis; Mastergradsoppgave, 2016-06-15)
      Steindalen er lokalisert sør på Lyngenhalvøya, i Troms fylke. Steindalsbreen er en av de lettest tilgjengelige breer i området. Dette gjør breen til et yndet turmål, men det gjør det også lettere å studere en bre på nært hold. Undersøkelse av Steindalsbreen har foregått ved hjelp av feltturer til området, ved å studere foto og flybilder over området og ved å sammenstille data samlet over mange år, ...
    • Bruddmønstre i øvre triaslagrekken ved Vindodden på Svalbard : opptreden, geometri og dannelsesmekanismer samt betydning for CO2 lagring 

      Wærum, Gard Ole (Master thesis; Mastergradsoppgave, 2011-05)
      Denne oppgaven beskriver et studie som ble gjennomført på nordsiden av Botneheiafjellet på Svalbard sommeren 2010. Målet med studiet var å analysere bruddmønstre i den øvre triaslagrekken, med ekstra fokus på: (1) De Geerdalenformasjonen som er reservoarbergart for CO2 injeksjon i ”Longyearbyen CO2 lab project”; (2) intrusive dolerittgangers bruddmønster og deres innvirkning på bruddutviklingen til ...
    • Caledonian nappe emplacement: an example from Uløya, Northern Norway 

      Kraus, Katrin (Master thesis; Mastergradsoppgave, 2016-06-27)
      On Uløya, an island located east of the Lyngen peninsula in northern Troms, Norway, four Caledonian nappes are exposed. These are from bottom to top: part of the Kalak Nappe Complex (KNC), the Vaddas, the Kåfjord and the Nordmannvik nappe. In the present study the geology of these nappes is described, macroscopic and microscopic deformation structures are analyzed, and phase equilibrium modeling is ...
    • Carbonate concretions in an ice-contact delta, Skarmunken, Ullsfjord, northern Norway 

      Amundsen, Mats (Master thesis; Mastergradsoppgave, 2017-03-10)
      At Skarmunken, a small village south of Ullsfjord, northern Troms, Norway, an outcrop containing carbonate concretions have been investigated. From sedimentary logging, five facies (facies A-E) have been classified by their grading and composition. Depositional data from logs, maximum pebble size (MPS) and earlier investigations suggests an ice-contact delta. TOC/TS data have revealed a dominantly ...
    • The Cenozoic pre-glacial sedimentary environment of the SW Barents Sea continental margin – Lofoten Basin 

      Høgseth, Gert Vidar (Master thesis; Mastergradsoppgave, 2016-05-15)
      2D seismic data have been analysed to study the Cenozoic pre-glacial sedimentary environment on the southwest Barents Sea margin and the Lofoten Basin. Based on a seismic stratigraphic analysis and correlation to previous work in the area, the pre-glacial seismic unit G0 has been subdivided into four. The four units have been described and discussed with regards to the geometry and internal seismic ...
    • Characterisation of palaeosols in the Lower Cretaceous Helvetiafjellet Formation, Svalbard. Palaeo-climatic implications 

      Tennvassås, Ingrid (Master thesis; Mastergradsoppgave, 2018-05-15)
      Although the Cretaceous period is known to have been dominated by greenhouse conditions, the Early Cretaceous climatic conditions in Svalbard have been under some debate. Both indicators of warm climate such as coal seams, Ornithopod tracks and warm-water dinoflagellates, and indicators of cold climate such as arctic belemnites, glendonites and ice rafted debris have been reported. This study ...
    • Characteristics and failure mechanisms of the unstable rock slope Dusnjárga 

      Bekkevoll, Simen (Mastergradsoppgave; Master thesis, 2022-05-15)
      Large slowly creeping rock slope deformations, with an annual displacement in the range of millimeters to centimeters, have been prone to rapid catastrophic failures in the past. This master thesis focuses on the unstable rock slope of Dusnjárga in Northern Norway. A sudden rapid failure of Dusnjárga would pose a threat to the local society in Lille Altafjord and Burfjord, due to potential secondary ...
    • Characterizing slope processes along the Piggtind mountain ridge, using 2D InSAR 

      Sandbakken, Henrik (Mastergradsoppgave; Master thesis, 2021-05-15)
      Large rock slope deformations potentially evolving into catastrophic rock avalanches pose an eminent threat to the Norwegian society. A comprehensive characterization of their kinematic behavior, progressive slope development, and current deformation rates are thus required for hazard management. Njunnás and Piggtind/Skulvatindane are two adjacent rock slopes located in Troms County, Norway. Both ...
    • Climate and sea-ice development between 890 and 1660 CE in SW Greenland revealed by marine diatom studies 

      Enguídanos, Eira Triguero (Master thesis; Mastergradsoppgave, 2022-11-24)
      This thesis presents the results of august Sea Surface Temperature reconstructions from marine diatom assemblages in samples from core Ga3-2 retrieved from Narsaq Sound, inside the Ikersuad fjord, South Greenland. The diatom samples provide a high-resolution (~30-year) reconstruction dating between 890 and 1660 CE (common era). The results show variable conditions with warm periods between 960 and ...
    • Climate controlled sedimentary processes in the Riiser Larsen Sea offshore Queen Maud Land, Antarctica 

      Brekken, Rita (Master thesis; Mastergradsoppgave, 2018-11-29)
      Multi-proxy analysis of gravity core PS56/029-1 have been performed in order to describe sedimentary processes and dynamics under pelagic, turbiditic and contouritic influences. The purpose is to reconstruct climate-controlled environmental change in the Riiser Larsen Sea, Antarctica, through past glacial/interglacial cycles. The gravity core was retrieved during expedition ANTARKTIS XVII/2 of R/V ...
    • Climate reconstruction during the Last Glacial Maximum based on a marine sediment core from Vestnesa Ridge, Svalbard 

      Matteis, Felix (Master thesis; Mastergradsoppgave, 2018-07-14)
      The sediment core HH15-1255PC has been analyzed to reconstruct the climate in the Fram Strait during the last 45,000 years. The coring site is located west of Svalbard on the Vestnesa Ridge, a contourite drift with a high-resolution sedimentary record (Plaza-Faverola et al., 2015). This ridge also includes a pockmark field formed by methane seepage (Vogt et al., 1994). The core HH15-1255PC is a ...
    • A combined 3D seismic and sedimentological study of the Lower Cretaceous succession in the northeastern part of the Nordkapp Basin 

      Brennhaugen, Adam Alfred (Master thesis; Mastergradsoppgave, 2018-05-15)
      In this master’s thesis in geology, 3D seismic data and shallow stratigraphic cores were used to investigate the Lower Cretaceous succession in the central sub-basin of the Nordkapp Basin, Barents Shelf. The Lower Cretaceous is listed as a potential petroleum play model on the Barents Shelf, which makes the succession of interest for petroleum exploration. Recent studies of the have divided the ...
    • Combining geophysical data with a mathematical model to describe vertical two-phase flow 

      Hansen, Johanne (Master thesis; Mastergradsoppgave, 2018-05-15)
      This thesis combines a geological model with a mathematical model to describe the vertical propagation of a gas plume through layers with different physical properties. The geological model is based on geophysical data from the Sørvestsnaget Basin and the mathematical model is derived based on the classical Buckley-Leverett theory for two-phase flow. The model estimates the velocity of a vertical ...
    • A comparative seismic study of gas chimney structures from active and dormant seepage sites offshore mid-Norway and west-Svalbard 

      Virs, Robert (Master thesis; Mastergradsoppgave, 2015-05-15)
      Understanding the fluid flow and the related fluid expulsion from gas chimneys and pipe structures is very important to our environment, since seeping methane has a great influence on our Earth’s climate. Chimneys are found in many places in the world, for instance at the Vestnesa ridge offshore western Svalbard and at the Nyegga region on the mid Norwegian margin. Plumbing systems and chimney ...
    • Comparison and classification of an Arctic Transitional snow climate in Tromsø, Norway 

      Velsand, Paul (Master thesis; Mastergradsoppgave, 2017-10-11)
      Winter tourism in Tromsø has increased significantly over the last years, consequently also the skiing tourism. It is advertised that Tromsø has a mild coastal climate compared to other destinations at similar latitudes. Existing snow climate classes separate covers into a maritime, continental and a transitional class where persistent weak layers are rare in the maritime class. Rain and average air ...
    • Comparison of 3D and 2D rockfall models. Considering terrain model quality effect on respective model performances 

      Hind, Håvard (Master thesis; Mastergradsoppgave, 2018-05-15)
      Rockfalls are blocks of rock that bounce and roll down slopes. They are commonly detached from rock-slopes with inclinations over 40-45°. They embody high energy and mobility and are a major cause of landslide related deaths. Rockfalls can be simulated using empirical relationships and modelling, of which 2D and 3D variants exist for the latter. 3D models allow for rock fragment- and surface shape ...
    • Connecting the late Neoproterozoic flysch sedimentation in the Gariep Belt (Namibia) with its potential source region in southern Dom Feliciano Belt (Uruguay) – a U-Pb detrital and protolith zircon study. 

      Gilberg, Ina Nordbø (Master thesis; Mastergradsoppgave, 2020-06-22)
      The Dom Feliciano Belt in Uruguay represents a counterpart of the Gariep Belt in Namibia and these two belts are presently considered as relics of one orogen split by the Atlantic Ocean. In this study, two presumed flysch samples from the Marmora Terrane of the Gariep Belt in Namibia, and five samples from potential source areas in the Nico Perez Terrane of the Dom Feliciano Belt in Uruguay have ...
    • Connection between chemical zonation and crystallographic preferred orientation as an indicator for the fabric development in eclogites. Example from the Saxothuringian eclogites, Bohemian massif, Czech Republic 

      Finstad, Ane Kongsro (Master thesis; Mastergradsoppgave, 2017-05-15)
      The presence of eclogites is one of the strongest evidences for high pressure metamorphism, and for the presence of a paleo subduction zone. Deformation of eclogites can yield important information about the kinematics of subduction zones. The main mechanism for fabric development in eclogites is still a matter of debate among various research groups and has split the field in two. Most previous ...