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Numerical Study on the Characteristics of AbyssalT-Wave Envelopes Controlled by Earthquake Source Parameters



Details

  • Journal Title:
    Seismological Research Letters
  • Personal Author:
  • NOAA Program & Office:
  • Description:
    Hydroacoustics has been successfully applied to detect and locate small-to-intermediate submarine tectonic activities infrequently recorded in land-based seismic arrays. However, to extend the utilization of T waves to extract other important earthquake source parameters, such as source strength, the roles of earthquake focal mechanisms, and source depths in T-wave envelopes must be thoroughly understood. We performed 3D numerical modeling considering anisotropic source radiation and realistic scattering in the oceanic crust for two focal mechanisms (normal and strike-slip faults) and three depths (5, 10, and 15 km) to investigate the effect of source radiation and focal depth on abyssal T waves. By analyzing the synthetic T-wave envelopes, we showed that stronger SV-energy radiation from a normal-fault earthquake event generates higher-intensity T waves of the same source magnitude. The anisotropic source radiation of a double-couple source causes azimuthal changes in the shapes of T waves, and deeper earthquakes cause gentle-sloped envelopes; however, the slopes also vary with respect to the azimuths of receivers and focal mechanisms. Temporal changes in the slopes of T-wave envelopes of magmatic swarm events near Wordie Volcano, Bransfield Strait, Antarctic Peninsula, imply that the depth dependency can be utilized to determine relative depths for hydrothermal-vent events or sequenced earthquakes.
  • Source:
    Seismological Research Letters, 93(4), 2189-2200
  • DOI:
  • ISSN:
    0895-0695 ; 1938-2057
  • Format:
  • Publisher:
  • Document Type:
  • Rights Information:
    Accepted Manuscript
  • Compliance:
    Submitted
  • Main Document Checksum:
    urn:sha-512:cec8de054b9b949a4c01aeaa395f6375ca7e7a7eff7fe72c4bb9e1e3d93ad55b35d3bc740acd452f280f045bae566f5c989b1a51a7caad745373f5190a55d8a0
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  • File Type:
    Filetype[PDF - 4.59 MB ]
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