The Tromsø University team was guided by colleagues from St. Petersburg State University headed by prof. Andrei Khudoley with logistics organized by North-East Federal University (Yakutsk). Artem Moiseev (Geological Institute RAS, Moscow) also participated in the trip.
During fieldtrip passive margin succession represented by Ordovician to Jurassic sedimentary rocks cut by rift-related Devonian and younger dykes and folded and faulted in Mesozoic was studied (picture below).
