Crustal Stresses in the East Arctic Region From New Data on Earthquake Focal Mechanisms.

Filippova, A. I.; Melnikova, V. I.

East Arctic is a key region for understanding the current geodynamic pattern and lithospheric evolution of the whole Arctic. To close an evident gap in regional seismic data, we calculate source parameters for 103 earthquakes (Mw ≥ 4.2, 1990–2021) and compile a representative uniform data set including source depths, scalar seismic moments, moment magnitudes, and focal mechanisms. On its basis, crustal stresses are estimated within four blocks with the homogeneous stress field. Extension dominates along the Gakkel Ridge and over most of the Laptev Sea shelf. On the continent and east and west of the shelf, it is replaced by compression. The obtained results indicate that the spreading axis of the Gakkel Ridge does not continue to the Laptev Sea shelf and evidence for the Eurasian–North American plate boundary crosses the eastern Laptev Sea shelf and is likely to pass to the Chersky Range through the Yana Bay. Plain Language Summary: Source parameters are calculated for 103 small‐to‐moderate earthquakes in East Arctic and crustal stresses are estimated and discussed on their basis. The obtained results partly fill an evident gap in seismic data in the Arctic. It is found that extension dominates along the Gakkel Ridge and over most of the Laptev Sea. On the continent and east and west of the shelf, it is replaced by compression. On the basis of the obtained results, we suggest that the spreading axis of the Gakkel Ridge does not continue to the Laptev Sea shelf and that the Eurasian–North American plate boundary crosses the eastern Laptev Sea shelf and is likely to pass to the Chersky Range through the Yana Bay. Key Points: Representative data set of earthquake source parameters (1990–2021) are compiled for East Arctic, crustal stresses are calculated from itThe results obtained indicate that the spreading axis of the Gakkel Ridge does not continue to the Laptev Sea shelfThe Eurasian‐North American plate boundary crosses the eastern Laptev Sea and is likely to pass to the Chersky Range through the Yana Bay

Tectonics, 2023, Vol 42, Issue 9, p1

0278-7407

Academic Journal

10.1029/2022TC007338