EGU25-21158, updated on 25 Apr 2025
https://doi.org/10.5194/egusphere-egu25-21158
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
The fluid-related short-duration events recorded by the OBS in the Mussau Trench
Yuan Wang1,2, Annan Ren1,2, Tianyao Hao1,2, Shengji Wei1, and Weidong Sun2,3
Yuan Wang et al.
  • 1Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing,1000292
  • 2University of Chinese Academy of Sciences,Beijing,100049
  • 3Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China

We have deployed 21 of our developed broad-band Ocean‐bottom seismometers (OBSs) along Mussau Trench in September 2024 with 100% recovery, and 19 OBSs recorded completed seismic data. A total of ~830 short‐duration events (SDEs) were picked manually after data preprocessing using the STA/LTA results. Commonly, the SDE seismic signal often described by all of these characteristics: (i) one single‐wave train with no identified P nor S wave arrivals, (ii) duration <1 s, and (iii) a dominant frequency usually between 4 and 30 Hz. In many areas, SDEs have been associated with gas‐ or fluid‐related processes near cold seeps or hydrothermal vents, although fish bumps, instrumental, or current‐generated noise have been proposed as possible sources. Our results show that the bending plate area has the largest number of SDE, which indicates strong hydrogen hydrothermal activities in this area. 

How to cite: Wang, Y., Ren, A., Hao, T., Wei, S., and Sun, W.: The fluid-related short-duration events recorded by the OBS in the Mussau Trench, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-21158, https://doi.org/10.5194/egusphere-egu25-21158, 2025.