• Beamforming of Rayleigh and Love Waves in the Course of Atlantic Cyclones 

      Pelaez Quiñones, J. D.ORCIDiD; Becker, D.ORCIDiD; Hadziioannou, C.ORCIDiD (Journal of Geophysical Research: Solid Earth, 2023-02-21)
      The main sources of the ambient seismic wavefield in the microseismic frequency band (peaking in the ∼0.04–0.5 Hz range) are earth's oceans, namely the wind‐driven surface gravity waves (SGW) that couple oscillations into ...
    • Temporal Modulation of the Local Microseism in the North Sea 

      Becker, D.ORCIDiD; Cristiano, L.; Peikert, J.; Kruse, T.; Dethof, F.; Hadziioannou, C.ORCIDiD; Meier, T. (Journal of Geophysical Research: Solid Earth, 2020)
      Primary and secondary microseism originating in the world oceans and peaking at around 14 and 7 s, respectively, characterize the Earth's background noise in that frequency range. Microseism generated in marginal seas with ...
    • Variation of Fault Creep Along the Overdue Istanbul‐Marmara Seismic Gap in NW Türkiye 

      Becker, D.ORCIDiD; Martínez‐Garzón, P.ORCIDiD; Wollin, C.ORCIDiD; Kılıç, T.; Bohnhoff, M.ORCIDiD (Geophysical Research Letters, 2023-03-22)
      Strain energy from tectonic loading can be partly released through aseismic creep. Earthquake repeaters, repeatedly activated brittle fault patches surrounded by creep, indicate steady‐state creep that affects the amount ...