Crustal structure of the Lofoten continental margin, off northern Norway, from ocean-bottom seismographic studies

In 1988, an extensive geophysical experiment was performed on the Lofoten passive continental margin, which was formed by the continental break-up between Greenland and northern Norway at 58 Ma. The geological units of the outer Lofoten margin are characterized by seaward-dipping reflectors (SDRs) a...

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Bibliographic Details
Published in:Geophysical Journal International
Main Authors: Kodaira, S., Goldschmidt-Rokita, A., Hartmann, J. M., Hirschleber, H. B., Iwasaki, T., Kanazawa, T., Krahn, H., Tomita, S., Shimamura, H.
Format: Text
Language:English
Published: Oxford University Press 1995
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Online Access:http://gji.oxfordjournals.org/cgi/content/short/121/3/907
https://doi.org/10.1111/j.1365-246X.1995.tb06447.x