Summary. The continental crust beneath the western Barents Sea has
been acoustically imaged down to Moho depths in a large scale deep
seismic reflection experiment. A first-order pattern of crustal reflectivity
has been established and the thickness of the crust determined. A
number of features with important implications for the tectonics
of the area have been discovered. The results are presented in the
form of two transects.
Department of Geology, University of Oslo, Norway; Continental Shelf
Institute (IKU), Trondheim, Norway; Esso Norge AS. Explor. and Prod.
Dep., Stavanger, Norway
year
1987
month
apr
journal
Geophysical Journal of the Royal Astronomical Society
%0 Journal Article
%1 gudlaugsson_etal:1987
%A Gudlaugsson, S.
%A Faleide, J.
%A Fanavoll, S.
%A Johansen, B.
%C Department of Geology, University of Oslo, Norway; Continental Shelf
Institute (IKU), Trondheim, Norway; Esso Norge AS. Explor. and Prod.
Dep., Stavanger, Norway
%D 1987
%I Blackwell Publishing Ltd
%J Geophysical Journal of the Royal Astronomical Society
%K geophysics seismics
%N 1
%P 273--278
%R 10.1111/j.1365-246X.1987.tb04419.x
%T Deep seismic reflection profiles across the western Barents Sea
%U http://dx.doi.org/10.1111/j.1365-246X.1987.tb04419.x
%V 89
%X Summary. The continental crust beneath the western Barents Sea has
been acoustically imaged down to Moho depths in a large scale deep
seismic reflection experiment. A first-order pattern of crustal reflectivity
has been established and the thickness of the crust determined. A
number of features with important implications for the tectonics
of the area have been discovered. The results are presented in the
form of two transects.
@article{gudlaugsson_etal:1987,
abstract = {Summary. The continental crust beneath the western Barents Sea has
been acoustically imaged down to Moho depths in a large scale deep
seismic reflection experiment. A first-order pattern of crustal reflectivity
has been established and the thickness of the crust determined. A
number of features with important implications for the tectonics
of the area have been discovered. The results are presented in the
form of two transects.},
added-at = {2012-09-01T13:08:21.000+0200},
address = {Department of Geology, University of Oslo, Norway; Continental Shelf
Institute (IKU), Trondheim, Norway; Esso Norge AS. Explor. and Prod.
Dep., Stavanger, Norway},
author = {Gudlaugsson, S. and Faleide, J. and Fanavoll, S. and Johansen, B.},
biburl = {https://www.bibsonomy.org/bibtex/2021844bb79e787bc4be445892953a0d3/nilsma},
doi = {10.1111/j.1365-246X.1987.tb04419.x},
interhash = {3d8a2c4ff4d48231cfe6dc01c963e3e0},
intrahash = {021844bb79e787bc4be445892953a0d3},
issn = {1365-246X},
journal = {Geophysical Journal of the Royal Astronomical Society},
keywords = {geophysics seismics},
month = apr,
number = 1,
pages = {273--278},
publisher = {Blackwell Publishing Ltd},
timestamp = {2021-02-09T13:27:42.000+0100},
title = {Deep seismic reflection profiles across the western Barents Sea},
url = {http://dx.doi.org/10.1111/j.1365-246X.1987.tb04419.x},
volume = 89,
year = 1987
}