Wu Y.; Louden K.E.; Funck T.; Jackson H.R.; Dehler S.A.(2006)
central Nova Scotia margin off Eastern Canada is located at a transition from a volcanic margin in the south to a non-volcanic margin in the north. In order to study this transition, a wide-angle refraction seismic line ...
Sorokin M.Yu.; Zamansky Yu.Ya.; Langinen A.Ye.; Jackson H.R.; Macnab R.(1999)
Wide-angle seismic reflection/refraction data, recorded on ten seismographs from five large explosive charges, clearly define the crustal and upper mantle velocities of the Makarov Basin. These data are combined with a ...