The Renlandian Orogeny is a Tonian (early Neoproterozoic) tectonic and metamorphic event that is found in East Greenland, on Svalbard, on Ellesmere Island and in Scotland. It takes its name from Renland in East Greenland, where the event was first recognised.[1]
- ^ Bird, A.; Cutts, K.; Strachan, R.; Thirlwall, M.F.; Hand, M. (2018). "First evidence of Renlandian (c. 950–940 Ma) orogeny in mainland Scotland: Implications for the status of the Moine Supergroup and circum-North Atlantic correlations". Precambrian Research. 305: 283–294. doi:10.1016/j.precamres.2017.12.019.