Post-Caledonian brittle faults along the SW Barents Sea Margin: onshore-offshore margin architecture and fault rock-forming conditions
Permanent lenke
https://hdl.handle.net/10037/7050Åpne
Thesis introduction (PDF)
Indrevær, K., Bergh, S.G., Koehl, J.-B., Hansen, J.-A., Schermer, E.R. & Ingebrigtsen, A.: ‘Post-Caledonian brittle fault zones on the hyperextended SW Barents Sea margin: New insights into onshore and offshore margin architecture’. Norwegian Journal of Geology, 2013, Vol 93 (3-4), pp. 167–188. ISSN 0029-196X. (PDF)
Indrevær, K., Stunitz, H., & Bergh, S. G.: 'On Palaeozoic-Mesozoic brittle normal faults along the SW Barents Sea margin: fault processes and implications for basement permeability and margin evolution'. This is the accepted manuscript version of the article. Published version in Journal of the Geological Society, London. v. 171 no. 6 p. 831-846. Available at http://dx.doi.org/10.1144/jgs2014-018 (PDF)
Indrevær, K. & Bergh, S. G.: ‘Linking onshore-offshore basement rock architecture and brittle faults on the submerged strandflat along the SW Barents Sea Margin using high-resolution (5x5m) bathymetry data’. This is the accepted manuscript version of the article. Published version in Norwegian Journal of Geology, 2014, Vol 94 (1), pp. 1-34. ISSN 0029-196X. (PDF)
Entire thesis in one comprehensive file (PDF)
Dato
2014-11-13Type
Doctoral thesisDoktorgradsavhandling
Forfatter
Indrevær, KjetilSammendrag
The thesis aims to unravel the evolution and finite stage architecture of the
SW Barents Sea Margin, which formed as a part of the rifting of present day Greenland and
Scandinavia and the opening of the North Atlantic Ocean (cf. Faleide et al., 2008). The SW
Barents Sea Margin studied in this thesis starts just north of the Lofoten-Vesterålen
archipelago, continues northward outboard northern Troms and into western Finnmark. This
thesis focus on (i) if and how onshore Post-Caledonian brittle faults correlate with major
offshore, basin-bounding fault complexes and (ii) under which conditions onshore faulting
occurred.
Forlag
UiT Norges arktiske universitetUiT The Arctic University of Norway
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