The ocean/continent transition along a profile through the Lofoten basin, Northern Norway

Author:

Goldschmidt-Rokita Andreas,Hansch Knut J. F.,Hirschleber Hans B.,Iwasaki Takaya,Kanazawa Toshihiko,Shimamura Hideki,Sellevoll Markvard A.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Oceanography

Reference27 articles.

1. ?ervený, V. and P?en?ík, I., 1983, SEIS 83?Numerical Modelling of Seismic Wave Field in Two Dimensional Lateral Varying Layered Structures by the Ray Method, in E. R. Engdahl,Documentation of Earthquake Algorithms, World Data Center (A) for Solid Earth Physics, Report SE-35: 36?40.

2. Dehghani, G. A., Hirschleber, H. B., Liebe, T., Gidskehaug, A., and Sellevoll, M. A., 1988, Magnetic Measurements on the Norwegian Continental Margin between 68° and 70° N,Dt. Hydrogr. Z. 41, H. 3?6.

3. Seismo-Series;G. A. Dehghani,1990

4. Drivenes, G., Sellevoll, M. A., Renard, V., Avedik, F., and Paichel, J., 1984, The Continental Margin/Crustal Structure off the Lofoten Islands, Northern Norway. In Spenceret al. (eds),Petroleum Geology of the North European Margin, Grahman and Trotman, London, pp. 211?216.

5. Eldholm, O., Thiede, J., Tayler, E.et al., 1989, Evolution of the Vøring Volcanic Margin, in O. Eldholm, J. Thiede, E. Tayleret al., Proc. ODP, Sci. Results, 104, College Station, TX (Ocean Drilling Program), pp. 1033?1065.

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