Implications for the geometry of plate boundaries in NE Asia based on the geodetic analysis of the 2020 M w 6.4 Koryak event

• Published in: Geophysical Journal International
• Main Authors: Svigkas, Nikos, Atzori, Simone, Kozhurin, Andrey, Tolomei, Cristiano, Antonioli, Andrea, Pezzo, Giuseppe
• Other Authors: European Space Agency, JAXA, Japan Aerospace Exploration Agency, United States Geological Survey, Ministry of Economic Development
• Format: Article in Journal/Newspaper
• Language: English
• Published: Oxford University Press (OUP) 2023
• Subjects: Geochemistry and Petrology; Geophysics; Bering Sea; Khatyrka; Vyvenka; Koryak
• Online Access: http://dx.doi.org/10.1093/gji/ggad142; https://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggad142/49706700/ggad142.pdf; https://academic.oup.com/gji/article-pdf/234/2/1412/49912603/ggad142.pdf

SUMMARY On the 9th of January 2020, an Mw 6.4 strike-slip earthquake took place north of the Asian margin of the Bering Sea. The earthquake occurred within the known reverse-right-lateral active fault zone, called Khatyrka–Vyvenka, which transverses the Koryak Highland from SE to NW and is thought to be a surface manifestation of the Asian portion of either the Bering plate boundary or the northern edge of the Alaskan stream. No other strong earthquake has ever been recorded in this remote uninhabited area and the few existing seismic stations provide poor quality earthquake locations. We adopt SAR interferometry (InSAR) technique to define an improved location of the Koryak 2020 earthquake and constrain the seismic source. The analysis of the 2020 event revealed a previously unknown active fault of left-lateral kinematics that is possibly hidden and strikes NW transversely to the Khatyrka–Vyvenka fault zone. Although several mechanisms could account for left-lateral kinematics of this fault, we propose that the structure is part of a more extended NW fault structure, that formed in pre-neotectonic times and has played a role of a pre-existing rheological discontinuity. This revived NW structure together with a similar structure located easterly, so far aseismic, make the plate/stream boundary segmented, step-like in plan view. The step-like boundary geometry may be the result of internal transform deformation of a rigid plate, but it is better explained by deflections of the Alaskan stream edge at local crustal asperities, which are pre-Cenozoic terrains.