Lithospheric Dynamics and Crustal Processes in Northern Europe
Summary
The lithosphere beneath Northern Europe comprises ancient cratonic blocks, Paleoproterozoic terranes and younger orogenic belts, all modified by Proterozoic–Palaeozoic tectonism and later intraplate processes. In Fennoscandia, the stable Precambrian shield has been shaped by Caledonian deformation and subsequent extensional regimes, notably the formation of the Oslo Rift. Deep seismic and tomographic investigations reveal a heterogeneous lithospheric mantle with pronounced velocity anomalies that correlate with surface topography and long‐lived terrane boundaries. Stratigraphic and geochronological studies of magmatic complexes in the Oslo Rift illustrate pulsed mafic–alkaline magmatism linked to lithospheric thinning and mantle upwelling. Heat‐flow and petrological data demonstrate that radiogenic crustal bodies and erosional cycles have controlled the thermal state of the upper crust, with implications for geothermal energy. Ongoing intraplate seismicity and crustal flexure reflect reactivation of ancient structures under far‐field stress. Together, these processes illustrate the interplay between deep mantle dynamics, crustal architecture and surface evolution in a region far from active plate margins.
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Lithospheric Dynamics and Crustal Processes in Northern Europe publication trend
The graph below shows the total number of articles in lithospheric dynamics and crustal processes in northern europe across all publications each year (not limited to Nature Index journals).
Technical terms
Lithosphere: The rigid outer shell of the Earth, including crust and uppermost mantle.
Asthenosphere: The mechanically weak, ductile layer beneath the lithosphere.
Craton: An ancient, stable block of continental lithosphere that has survived cycles of deformation.
Tomography: A technique for imaging internal Earth structures by inverting seismic wave data.
Receiver function: A seismic analysis method that isolates converted phases to infer crustal discontinuities such as the Mohorovičić (Moho) boundary.
References
- Timing and Petrogenesis of the Permo-Carboniferous Larvik Plutonic Complex, Oslo Rift, Norway: New Insights from U–Pb, Lu-Hf, and O Isotopes in Zircon. Journal of Petrology (2022).
- Some remarks on the earthquakes of Fennoscandia: A conceptual seismological model drawn from the perspective of hyperextension. Norwegian Journal of Geology (2015).
- Seismic probing of buried ancient terrane boundaries - insight into Fennoscandia’s Palaeoproterozoic continental formation. Precambrian Research (2024).
- The deep geothermal potential of the radiogenic Løvstakken Granite in western Norway. Norwegian Journal of Geology (2020).
- Highly heterogeneous upper-mantle structure in Fennoscandia from finite-frequency P-body-wave tomography. Geophysical Journal International (2022).
- New heat flow data from the Veiholmen and Raudsand boreholes, middle Norway. Geothermics (2021).
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