One seep anomaly was noted relatively close to the major basaltic eruptive complex near the Gjoa G-
37 well. This may be due to the presence of volcaniclastic- hosted hydrocarbons similar in style to those
recently discovered at the Rosebank field in Paleocene volcanics in the Faroe-Shetland Basin. The
occurrence of an active seep in a volcanically-dominated terrain raises the potential for a radical shift in
accepted types of petroleum leads and where they may occur