Crustal structure and intraplate seismicity in Nordland, Northern Norway: insight from seismic tomography

• Published in: Geophysical Journal International
• Main Authors: Shiddiqi, H A, Ottemöller, L, Rondenay, S, Halpaap, F, Gradmann, S, Michálek, J
• Other Authors: Research Council of Norway
• Format: Article in Journal/Newspaper
• Language: English
• Published: Oxford University Press (OUP) 2022
• Subjects: Nordland; North Atlantic; Northern Norway
• Online Access: http://dx.doi.org/10.1093/gji/ggac086; https://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggac086/42619317/ggac086.pdf; https://academic.oup.com/gji/article-pdf/230/2/813/43373196/ggac086.pdf

SUMMARY The Nordland region, Northern Norway, situated in an intraplate continental setting, has the highest seismicity rate in mainland Norway. However, the exact cause of seismicity in this region is still debated. Better understanding of factors that influence the seismicity in Nordland can help increase knowledge of intraplate seismicity in general. Here, we address this problem with the aid of a new high-resolution 3-D VP and VP/VS ratio images of the crust in Nordland using seismic traveltime tomography. These images show the existence of a localized, 10–15 km Moho step that runs parallel to the coast. The north–south extent of this step coincides with the region that exhibits the highest rates of seismicity. Focal mechanisms of selected earthquakes computed in this study are dominated by normal and oblique-normal, indicating a coast-perpendicular extension. The coast-perpendicular extensional stress regime deviates from the regional compression imposed by the ridge push from the North Atlantic. This deviation is thought to stem from the additional interference with local flexural stress caused by sediment redistribution and glacial isostatic adjustment, and possibly exacerbated by gravitational potential energy stress associated with the Moho step. The deformation due to the extensional regime is localized on pre-existing faults and fractures along the coastline. The tomography result shows that two distinct seismic swarms occurred in the coastal area with low VP and variable VP/VS ratio anomalies, pointing towards fractured crust and possibly the presence of fluids. The existence of fluids here can change the differential stress and promote seismic rupture.