A Review of the Spatiotemporal Evolution of the High Arctic Large Igneous Province, and a New U-Pb Age of a Mafic Sill Complex on Svalbard
The High Arctic Large Igneous Province (HALIP) formed in the circum-Arctic during the Cretaceous. The timing and duration of emplacement of these mafic magmas are important for understanding the climatic and environmental effects, yet many uncertainties remain. The dating methods used vary greatly between different regions. For example, the mafic intrusions in Svalbard have mainly been dated using
