Journal of Tropical Oceanography ›› 2022, Vol. 41 ›› Issue (5): 57-63.doi: 10.11978/2021178CSTR: 32234.14.2021178

Special Issue: 台湾海峡专题

• Marine Geophysics • Previous Articles     Next Articles

Characteristics of secondary Ps phases recorded by ocean bottom seismometer in the Taiwan Strait and its application

GUO Xiaoran(), LIU Shanhu   

  1. Xiamen Institute of Marine Earthquake, China Earthquake Administration, Xiamen 361021, China
  • Received:2021-12-22 Revised:2022-01-28 Online:2022-09-10 Published:2022-02-13
  • Contact: GUO Xiaoran E-mail:gxr19890902@126.com
  • Supported by:
    Youth Science and Technology Fund of Earthquake Administration of Fujian Province(Y202001)

Abstract:

On the ocean bottom seismometer (OBS) wide-angle seismic record section, multiple signals with high energy and good continuity can often be detected. As same as the first arrival phases, multiple phases also can be real reflections of subsurface interfaces, they are generated by the same source signal. However, in the conventional OBS data processing, multiple signs are often deleted as invalid signals, just a few studies are concerned with their properties and applications. By processing the OBS data acquired from Line HXN01 in the southern Taiwan Strait, the secondary phases are identified and picked on eight seismic recording sections. Analysis of the measured data from OBS0106 station reveals that the waveform characteristics and particle motion trajectory of these two phases are very similar, the amplitude of the secondary Ps phases is greater than that of the first arrival phases. Then we determined that the secondary reflecting interface corresponds to the secondary Ps phases by Rayinvr ray tracing simulation. The fitting results of travel time shows that after adding the secondary phases, the ray-coverage density of the shallow sedimentary layer under the station is significantly increased, and the ray-coverage area is also significantly increased, which provides more information for the inversion of sedimentary structure. In addition, the inversion test before and after the addition of the secondary Ps phase was performed on the crustal structure of the theoretical model, and it was found that after the addition of the secondary Ps phase data, the interface depth error of the sedimentary layer improved significantly.

Key words: ocean bottom seismometer (OBS), secondary Ps phases, Taiwan Strait, crustal structure

CLC Number: 

  • P712.83