Now showing items 1-4 of 4

  • The continent-ocean crustal transition across the southwest Greenland margin 

    This article first appeared in:: Chian, Deping, and K. E. Louden. 1994. "The continent-ocean crustal transition across the southwest Greenland margin." Journal of Geophysical Research 99: 9117-35. DOI: 10.1029/93JB03404
    The complete crustal transition across the nonvolcanic, southwest Greenland continental margin of the Labrador Sea is examined using wide-angle and coincident vertical-incidence seismic profiles. Six ocean bottom seismometers ...
  • Extinct spreading center in the Labrador Sea: Crustal structure from a two-dimensional seismic refraction velocity model 

    Osler, J. C., and K. E. Louden. 1995. "Extinct spreading center in the Labrador Sea: Crustal structure from a two-dimensional seismic refraction velocity model." Journal of Geophysical Research 100: 2261-78. DOI: 10.1029/94JB02890
    The Labrador Sea contains a rare example of an abandoned mid-ocean ridge where active accretion of oceanic crust ceased due to a change in the spreading geometry of lithospheric plates. Seismic refraction data were collected ...
  • Heat flow in the Balearic and Tyrrhenian basins, western Mediterranean 

    This article first appeared in: Hutchison, I., R. P. Von Herzen, K. E. Louden, J. G. Sclater, et al. 1985. "Heat flow in the Balearic and Tyrrhenian basins, western Mediterranean." Journal of Geophysical Research 90: 685-701. DOI: 10.1029/JB090iB01p00685
    Presents the results of three detailed heat flow surveys which are used to investigate the variations of heat flow and age of the Balearic and Tyrrhenian basins in the western Mediterranean. The heat flow values are within ...
  • Variations in heat flow across the Goban Spur and Galicia Bank continental margins 

    Louden, K. E., J. -C Sibuet, and J. -P Foucher. 1991. "Variations in heat flow across the Goban Spur and Galicia Bank continental margins." Journal of Geophysical Research 96: 16131-50. DOI: 10.1029/91JB01453
    Presents the results of 44 new heat flow stations which were taken in 1984 and 1989 in profiles across the Goban Spur and Galicia Bank continental margins (NE Atlantic Ocean). Simple extensional models indicate that the ...