| Summary: | Paper number 1 and 2 of the thesis are not available in Munin due to publishers' restrictions: 1. Plaza-Faverola, A., S. Bünz, and J. Mienert (2010). "Fluid distributions inferred from Pwave velocity and reflection seismic amplitude anomalies beneath the Nyegga pockmark field of the mid-Norwegian margin", Marine and Petroleum Geology, 27(1): 46-60 2. Plaza-Faverola, A., G. K. Westbrook, K. Stephan, R. Exley, A. Gailler, T. Minshull and K. Broto, (2010). "Evidence from tomographic investigation of Vp variation for accumulation of substantial methane hydrate in a fluid-escape chimney in the Nyegga pockmark field, offshore Norway". JGR solid earth. v. doi:10.1029/2009JB007078 , in press. What causes the escape of natural gases to the seafloor and how significant this escape has been along the mid-Norwegian continental margin? These are questions that guided the doctoral thesis. The thesis is part of a research project supported by the European Commission and the Norwegian Research Council, which aims at quantifying geological processes that control fluid flow and gas hydrate formation along the Norwegian-Barents-Svalbard margin. The thesis was divided in three stages according to the following three main objectives: (1) to assess the distribution of shallow gas reservoirs and paths for fluid migration from deep sources; (2) to investigate the internal structure of a vertical fluid escape feature (chimney) through implementation of high resolution travel-time reflection tomography modeling; and (3) to infer a time scale for fluid escape in the region through detailed seismic characterization of depositional settings and sediment deformation of sediments deposited during the last three major glaciations and their inter-glacial cycles. The methodology implemented consists in the integration of velocity analysis techniques and seismic imagine applied to different resolution seismic data sets. The thesis presents results from four articles that together bring us closer to the overall understanding of fluid flow ...
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