Institutt for geovitenskap: Nye registreringer
Viser treff 881-900 av 1012
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Effects of mortality changes on biomass and production in Calanus spp. populations
(Journal article; Tidsskriftartikkel; Peer reviewed, 2011-04-28)Calanus species are the main link between primary producers and higher trophic-level organisms in the Barents Sea. The natural mortality rate is an essential parameter for determining the standing stock of Calanus, but it is also one of the most uncertain parameters in present knowledge. The level of human activity, and the associated risk of pollution, is increasing in the Barents Sea, and knowledge ... -
Land sokkel korrelasjon av sprø mesozoiske og paleozoiske forkastninger i et profil over Vestfjordbassenget, Vestvågøya og Ribbebassenget.
(Master thesis; Mastergradsoppgave, 2015-08-19)Denne studien har studert geomorfologi og sprø forkastninger i et profil som strekker seg fra Vestfjordbassenget, over Vestvågøya/Lofotryggen og Ribbebassenget. Det flate slettelandskapet sentralt på Vestvågøya skiller seg ut fra landskapet ellers i Lofoten, som stor sett består av alpint fjellandskap. Slettelandskapet er omgitt av alpine asymmetriske fjell langs kysten i NØ og NV. Fjellenes brattside ... -
Analyse av mesozoiske forkastninger og asymmetriske landskap i et profil over Lofotryggen ved Leknes, Vestvågøy. Implikasjoner for dannelsen av roterte forkastningsblokker, riftrelaterte bassenger og nedforkastningen av Leknesgruppen
(Master thesis; Mastergradsoppgave, 2015-07-15)Dette studiet fokuserer på asymmetriske landskap og deres relasjon til sprø forkastninger, bassenger og roterte forkastningsblokker i et profil over Lofotryggen ved Leknes. Det anvendte datasettet består av sammensatte data fra feltarbeid og landskapsobservasjoner, batymatriske kart og seismiske profiler fra kontinentalsokkelen i Lofoten og Vesterålen. Lofotryggen er definert av to prominente NØ-SV ... -
Study of the Late Cenozoic depositional environment and seismic anomalies on the Trøndelag Platform using 3D seismic data
(Master thesis; Mastergradsoppgave, 2015-06-04)This thesis has focused on the depositional environment during the development of the Naust Formation in order to improve our understanding of the glacial history of the mid-Norwegian continental shelf, using 3D-seismic data from the Trænabanken and Sklinnadjupet area along with regional 2D-lines. Seismic anomalies have also been investigated to increase our understanding of fluid migration affecting ... -
Geomorphological study of the rock-slope failure at Adjet, Storfjord, Troms
(Master thesis; Mastergradsoppgave, 2015-06-06)Norway is known for its steep mountains and many fjords. This landscape provides the potential for large rock-slope failures (RSFs) which, in turn, can cause other catastrophic hazards, e.g. tsunamis. In Troms County, northern Norway, many RSFs are found east and west of the Lyngen peninsula, within an area of discontinuous permafrost. The RSF at Adjet is located southeast of the Lyngen peninsula. ... -
High-resolution study of selected Dansgaard- Oeschger events and Heinrich event 4 42,189–33,393 cal. years BP. Gravity core JM11-FI-15GC from Fugløy Ridge, northeastern Faeroe Islands Margin
(Master thesis; Mastergradsoppgave, 2015-05-15)The focus of this thesis was selected Dansgaard-Oeschger (D-O) events and Heinrich event 4 (H4). A gravity core, JM11-FI-15GC, from Fugløy Ridge was used for the investigation. The location of the core site is important due the fact that the Faeroe- Shetland Channel is a key area in understanding the changes in circulation during the last glacial period. In total there were eighteen D-O climatic ... -
Structural and geochemical mapping of a Fe-mineralized quartz-mica rich unit in the Ringvassøya Greenstone Belt, West Troms Basement Complex
(Master thesis; Mastergradsoppgave, 2015-05-28)Ringvassøy is one of a chain of large coastal islands representing the Archaean to Paleoproterozoic West Troms Basement Complex (WTBC), west of the Caledonides. On Ringvassøy, a basement of mainly tonalitic gneiss is overlain by the Ringvassøy Greenstone Belt (RGB), which is metamorphosed up to middle amphibolite facies. Tonalitic gneiss in the west and southeast of the island has U–Pb zircon ages ... -
Dannelse og utvikling av submarine kanjoner på kontinentalskråningen utenfor Lofoten
(Master thesis; Mastergradsoppgave, 2015-05-15)Tre kanjoner på kontinentalskråningen utenfor Lofoten er studert ut fra multistråle batymetridata, høyoppløselig seismiske data og foto av havbunnssedimenter. Formålet med denne studien er å diskutere dannelse, utviklingen av og den yngste aktiviteten i de tre kanjonene. To hovedhypoteser vedrørende kanjoners dannelse råder i dag; dannelse fra bunn av kontinentalskråningen og oppover eller fra ... -
A comparative seismic study of gas chimney structures from active and dormant seepage sites offshore mid-Norway and west-Svalbard
(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 ... -
Reconstruction of Holocene Paleoenvironment in Smeerenburgfjorden, northwest Svalbard based on benthic foraminifera and sedimentological investigations
(Master thesis; Mastergradsoppgave, 2015-05-16)Two gravity cores JM06-024-GC3 and JM07-049-GC1 from Smeerenburgfjorden at the northwestern corner of Svalbard have been investigated for the distribution pattern of the benthic foraminiferal faunas. The oxygen and carbon isotope values in benthic foraminifera were analysed and together with other proxy data such as ice rafted debris (IRD), were used in order to reconstruct the paleoceanography and ... -
Sedimentary processes and paleoenvironments in Moskusoksefjord and Nordfjord, North-East Greenland.
(Master thesis; Mastergradsoppgave, 2015-05-15)Multi-proxy analyses of five sediment cores (including lithostratigraphy, physical properties and XRF-scanning) and analyses of swath bathymetry and high resolution seismic data were integrated in order to reconstruct the Holocene glacial history and paleoenvironment of Moskusoksefjord and inner parts of Nordfjord, North-East Greenland. In Moskusoksefjord, the large-scale bathymetry is divided ... -
A shallow gas flat spot anomaly in the Bjørnøyrenna Fault Complex in the Barents Sea: processing and interpretation of P-Cable 3D seismic data
(Master thesis; Mastergradsoppgave, 2015-05-18)This thesis analyzed P-Cable high-resolution 3D seismic data from the Bear Island Fault Complex in the southwestern Barents Sea acquired during a Helmer Hanssen cruise in 2012. Hence, the thesis is divided into two parts: the first part of the thesis focuses on the steps taken during the processing of the raw seismic data from the Lundin 2012 Area-A survey located at the Bear Island Trough Fault ... -
Undersøkelse av ustabilt fjellparti ved Adjet, Storfjord, Troms. Betydningen av ulike kategorier av glideplan i berggrunnen og mekanismer for utglidning
(Master thesis; Mastergradsoppgave, 2015-05-15)Strukturelle element i berggrunnen kan ha stor betydning for utvikling av ustabile fjellparti og fjellskred. I dette studiet vil det fokuseres på hvilken rolle strukturelle element i berggrunnen har hatt å si for skredhendelsene og deformasjonen i området og hvordan disse har preget det geologiske bildet. Det ustabile fjellpartiet er lokalisert på fjellet Adjet ved tettstedet Skibotn i Storfjord ... -
Sedimentary processes and paleoenvironments in St. Jonsfjorden, western Spitsbergen
(Master thesis; Mastergradsoppgave, 2015-05-19)Multibeam (swath) bathymetry, high-resolution two-dimensional seismic (chirp) profiles and four gravity cores have been analyzed to reconstruct the Late Weichselian and Holocene sedimentary environments and glacier dynamics in St Jonsfjorden, central western Spitsbergen (Svalbard). The sediment cores comprise stratified glacimarine sediments with varying amounts of ice rafted debris. Three cores ... -
Faulting and the relationship to fluid migration and shallow gas accumulation in the Hammerfest Basin, SW Barents Sea
(Master thesis; Mastergradsoppgave, 2015-05-01)This thesis has focused its efforts to identify and map faults and their relationships to shallow gas accumulations and fluid flow features. The area of this investigation lies in the hydrocarbon-prone Hammerfest Basin in the southwestern Barents Sea, above the Base Cretaceous. Nine 3D seismic datasets were used in this study, aiming to improve the knowledge of the timing of the tectonic activity ... -
Asynchronous response of marine-terminating outlet glaciers during deglaciation of the Fennoscandian Ice Sheet
(Journal article; Tidsskriftartikkel; Peer reviewed, 2014-03-31)Recent studies have highlighted the dynamic behavior of marine-terminating outlet glaciers over decadal time scales, linked to both atmospheric and oceanic warming. This helps explain episodes of nearly synchronous fl ow acceleration, thinning, and retreat, but nonclimatic factors such as changes in fjord width and depth, can also induce rapid recession. There is support for these topographic ... -
Geomorfologisk og strukturgeologisk studium av fjellskredet ved Falsnesfjellet, Storfjord, Troms
(Master thesis; Mastergradsoppgave, 2014-04-08)Geomorfologisk og strukturgeologisk studium av fjellskredet ved Falsnesfjellet, Storfjord, Troms -
Optimising the use of marine tephrochronology in the North Atlantic: a detailed investigation of the Faroe Marine Ash Zones II, III and IV
(Journal article; Tidsskriftartikkel; Peer reviewed, 2014) -
A North Atlantic tephrostratigraphical framework for 130–60 ka b2k: new tephra discoveries, marine-based correlations, and future challenges
(Journal article; Tidsskriftartikkel; Peer reviewed, 2014) -
Temporal and spatial structure of multi-millennial temperature changes at high latitudes during the Last Interglacial
(Journal article; Tidsskriftartikkel; Peer reviewed, 2014)