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).
![R Ndi Ka -KZp Avw 1TCpzr UE4-t P3FOxeb 3U34CSdf Mb LI (1)](https://ua.vps03.fwstatic.download/media/1261869/rndika-kzpavw1tcpzrue4-tp3foxeb3u34csdfmbli_499x333.jpg)