Seismic imaging and velocity structure around the JFAST drill site in the Japan Trench: low Vp, high Vp/Vs in the transparent frontal prism

• Published in: Earth, planets, and space Vol. 66; no. 1; pp. 1 - 12
• Main Authors: Nakamura, Yasuyuki, Kodaira, Shuichi, Cook, Becky J, Jeppson, Tamara, Kasaya, Takafumi, Yamamoto, Yojiro, Hashimoto, Yoshitaka, Yamaguchi, Mika, Obana, Koichiro, Fujie, Gou
• Format: Journal Article
• Language: English
• Published: Heidelberg Springer Nature B.V 01.12.2014; BioMed Central Ltd
• Subjects: Coring; Ocean models; P waves; Prisms; Reflection; Seismic surveys; Trenches; INW, Pacific, Japan Trench
• ISSN: 1880-5981; 1880-5981
• DOI: 10.1186/1880-5981-66-121

Seismic image and velocity models were obtained from a newly conducted seismic survey around the Integrated Ocean Drilling Program (IODP) Japan Trench Fast Drilling Project (JFAST) drill site in the Japan Trench. Pre-stack depth migration (PSDM) analysis was applied to the multichannel seismic reflection data to produce an accurate depth seismic profile together with a P wave velocity model along a line that crosses the JFAST site location. The seismic profile images the subduction zone at a regional scale. The frontal prism where the drill site is located corresponds to a typically seismically transparent (or chaotic) zone with several landward-dipping semi-continuous reflections. The boundary between the Cretaceous backstop and the frontal prism is marked by a prominent landward-dipping reflection. The P wave velocity model derived from the PSDM analysis shows low velocity in the frontal prism and velocity reversal across the backstop interface. The PSDM velocity model around the drill site is similar to the P wave velocity model calculated from the ocean bottom seismograph (OBS) data and agrees with the P wave velocities measured from the core experiments. The average Vp/Vs in the hanging wall sediments around the drill site, as derived from OBS data, is significantly larger than that obtained from core sample measurements.