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Blar i Department of Earth Science på tittel 
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  • Blar i Department of Earth Science på tittel
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  • Faculty of Mathematics and Natural Sciences
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  • Department of Earth Science
  • Blar i Department of Earth Science på tittel
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Blar i Department of Earth Science på tittel

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    • Development of Gilbert-type deltas: sedimentological case studies from the Plio-Pleistocene of Corinth Rift, Greece 

      Gobo, Katarina (Doctoral thesis, 2014-05-28)
      Gilbert-type deltas form where a river system debouches into a relatively deep marine or lacustrine basin, whereby the subaqueous delta slope is steep and fully dominated by sediment gravity-transport processes. These ...
    • The development of oxygen content in the Greenland Sea from 1993 to 2008. A study of convection depth and deep layer changes. 

      Botnen, Helle Augdal (Master thesis, 2009-05-25)
      In previous years the hydrography in the Greenland Sea have been investigated based on temperature and salinity observations along with different transient tracers. In this work annual zonal sections, averaged values of ...
    • The Diagenesis and porosity of the mixed deposits of the Azagador Member (U. Miocene) in the Turre Area, Almeria, Spain 

      Enge, Håvard H. (Master thesis, 2002)
    • Diagnostics of seismic time-lapse effects of sandstones based on laboratory data 

      Moyano, Bernardo; Johansen, Tor Arne; Agersborg, Remy; Spikes, Kyle Thomas (Peer reviewed; Journal article, 2014-09)
      We evaluated a viscoelastic modeling of P- and S-wave velocity dispersion, attenuation, pressure, and fluid effects for a set of siliciclastic rock samples. Our analysis used a published laboratory data set of 63 sandstones ...
    • Dinoflagellate cyst stratigraphy and palaeoenvironment of the "Utsira Sand" in the northern North Sea 

      Al-Saadi, Lubna Sami Jawad (Master thesis, 2014-11-20)
      Safe CO_2 storage in the Utsira Formation is one of many solutions to climate change mitigation. A major leakage had occurred in the Utsira Formation in 2008, due to water injection in what was believed to be the Utsira ...
    • Direct image-to-geometry registration using mobile sensor data 

      Kehl, Christian; Buckley, Simon John; Gawthorpe, Robert; Viola, Ivan; Howell, John Anthony (Peer reviewed; Journal article, 2016)
      Adding supplementary texture and 2D image-based annotations to 3D surface models is a useful next step for domain specialists to make use of photorealistic products of laser scanning and photogrammetry. This requires a ...
    • The discovery of the Younger Dryas, and comments on the current meaning and usage of the term 

      Mangerud, Jan (Journal article; Peer reviewed, 2021)
      The Younger Dryas (YD) cold event was discovered in Denmark by Hartz and Mithers in 1904 and the term coined by Hartz in 1912. It was identified as a lacustrine clay bed containing plant macrofossils of an Arctic flora, ...
    • Disentangling rock record bias and common-cause from redundancy in the British fossil record 

      Dunhill, Alexander M.; Hannisdal, Bjarte; Benton, Michael J. (Peer reviewed; Journal article, 2014-09-04)
      The fossil record documents the history of life, but the reliability of that record has often been questioned. Spatiotemporal variability in sedimentary rock volume, sampling and research effort especially frustrates ...
    • Disentangling source of moisture driving glacier dynamics and identification of 8.2 ka event: evidence from pore water isotopes, Western Himalaya 

      Kumar, Om; Ramanathan, Al L.; Bakke, Jostein; Kotlia, Bata; Shrivastava, J. P. (Journal article; Peer reviewed, 2020)
      Two atmospheric circulation patterns, the Indian Summer Monsoon (ISM) and mid-latitude Westerlies control precipitation and thus glacier variability in the Himalaya. However, the role of the ISM and westerlies in controlling ...
    • Dissolved gases in hydrothermal plumes from Artic vent fields 

      Stensland, Anne (Master thesis, 2013-10-30)
      Recent discoveries of active vent fields on slow and ultraslow spreading ridges have revealed that hydrothermal activity is more common than previously assumed. In the Norwegian-Greenland Sea, two such vent fields are ...
    • Distribution of deformation associated with relay and tip damage zones of normal faults - a case study from Kilve, UK 

      Vaagan, Siri (Master thesis, 2017-06-13)
      The aim of this study is to investigate and characterize distribution of deformation and damage associated with relays and tips of normal faults at a range of scales. This is done through field based studies and digital ...
    • The distribution of rivers to terrestrial sinks: Implications for sediment routing systems 

      Burr Nyberg, Bjørn; Gawthorpe, Rob; Helland-Hansen, William (Peer reviewed; Journal article, 2018-09)
      Empirical observations used to constrain controls on large global modern river systems typically use catchment delineations depicting drainage patterns of rivers to oceans. A key component in the spatial and temporal ...
    • Distribution of thermochemical output and associated ecosystems at the Loki’s Castle hydrothermal field 

      Rikter-Svendsen, Rasmus (Master thesis, 2020-12-04)
      Loki’s Castle is a hydrothermal vent field situated on the ultra-slow Arctic mid-Ocean ridges, at the boundary of the Mohns- and Knipovich segments (73◦30’N, 08◦E), and consists of two sulfide mounds and associated black ...
    • Do deformation bands matter forflow? Insights from permeability measurements and flow simulations in porous carbonate rocks 

      Rotevatn, Atle; Fossmark, Heidi Synnøve Solli; Bastesen, Eivind; Thorsheim, Elin; Torabi, Anita (Peer reviewed; Journal article, 2017-02)
      We investigate the permeability and flow effects of deformation bands in porous granular carbonate rocks in Malta and use results from flow simulations to discuss the practical implications of deformation bands in carbonate ...
    • Double-Difference Relocation and Empirical Green’s Function Analysis of Storfjorden Earthquakes 

      Tjåland, Norunn (Master thesis, 2017-06-08)
      On 21 February 2008, an earthquake of magnitude Mw 6.1 occurred in Storfjorden on Svalbard. Since then, more than 2000 earthquakes have been recorded in this region. More recently, on 29 March 2016, an earthquake of magnitude ...
    • Down-dip correlation and modelling of shallow-marine and estuarine deposits in the Sunnyside Member, Book Cliffs, Eastern Utah: implications for the formation of non-depositional discontinuity surfaces 

      Sømme, Tor Oftedal (Master thesis, 2005-11)
      The Sunnyside Member is part of the Blackhawk Formation and consists of shallow-marine and estuarine deposits reflecting high-frequency changes in sea level. Detailed mapping of the unit reveals an intra parasequence ...
    • Drainage integration and sediment dispersal in active continental rifts: A numerical modelling study of the central Italian Apennines 

      Cowie, Patience; Duclaux, Guillaume; Gawthorpe, Rob; Huismans, Ritske; Pedersen, Vivi; Wedmore, Luke; Geurts, Anneleen H. (Journal article; Peer reviewed, 2018)
      Progressive integration of drainage networks during active crustal extension is observed in continental areas around the globe. This phenomenon is often explained in terms of headward erosion, controlled by the distance ...
    • Drilling for the Archean Roots of Life and Tectonic Earth in the Barberton Mountains 

      Grosch, Eugene; McLoughlin, Nicola; de Wit, Maarten; Furnes, Harald (Peer reviewed; Journal article, 2009)
    • Drumlin relief 

      Spagnolo, Matteo; Clark, Chris D.; Hughes, Anna L.C. (Peer reviewed; Journal article, 2012)
      Drumlin relief is a key parameter for testing predictions of models of drumlin formation. Although this metric is commonly described in textbooks as being of the order of a fewtens ofmetres, our critical review of the ...
    • Dynamic Topography Development North of Iceland from Subaerial Exposure of the Igneous Logi Ridge, NE Atlantic 

      Tan, Pingchuan; Breivik, Asbjørn Johan; Mjelde, Rolf (Peer reviewed; Journal article, 2019)
      The Logi Ridge, located north of the West Jan Mayen Fracture Zone, is E-W oriented and 140-150 km long. The seafloor surrounding the Logi Ridge is ~0.65 km shallower than the conjugate seafloor east of the Mohn’s Ridge, ...

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