气候变化领域集成服务门户(CCPortal): 2D spatial distribution of reflection intensity on the upper surface of the Philippine Sea plate off the Boso Peninsula, Japan

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DOI	10.1016/j.tecto.2019.228206
	2D spatial distribution of reflection intensity on the upper surface of the Philippine Sea plate off the Boso Peninsula, Japan
	Kono A.; Sato T.; Shinohara M.; Mochizuki K.; Yamada T.; Uehira K.; Shinbo T.; Machida Y.; Hino R.; Azuma R.
发表日期	2020
ISSN	00401951
卷号	774
英文摘要	The region off the Boso Peninsula, Japan, is a tectonically complex area where the Pacific plate is subducting beneath both the landward plate and the Philippine Sea plate (PHS) from the Japan trench and the Izu-Bonin trench as the PHS is subducting under the landward plate from the Sagami trough. It is important to better determine the structure of this region to deepen our understanding of its seismicity. Previous seismic reflection studies have shown that reflections from the upper surface of the PHS vary with depth, being stronger in the main slip area of the slow slip events beneath the Boso Peninsula (Boso SSEs). However, the spatial relationship between the reflective area and the SSEs is poorly constrained. This study mapped the distribution of the reflective area using data recorded by ocean bottom seismometers during an active-source seismic experiment. We constructed a 3D P-wave velocity structure by using traveltimes of first arrivals from 18 ocean bottom seismometer records. We also adapted the traveltime mapping method to reflection traveltimes, projecting them to the depth–distance domain, to map the 2D distribution of strong reflections from the top of the PHS. These reflections were concentrated in two areas, one near the main slip area of the Boso SSEs and the other about 60 km to the east. In the first area, the absence of strong velocity contrasts near the top of the PHS suggests that the reflections were generated by a thin low-velocity layer. In contrast, the structure of the second area has a convex shape of high velocity with a high velocity gradient near the top of the PHS. This structure may represent boninitic material of the outer-arc high, partially serpentinized peridotite, or gabbro displaced by intraoceanic reverse faults. © 2019 The Author(s)
关键词	3D P-wave velocity structure Boso slow slip events (SSEs)Izu-Bonin arc Ocean bottom seismometers (OBSs)Philippine Sea plate Traveltime mapping
语种	英语
来源期刊	Tectonophysics
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/207795
作者单位	Graduate School of Science, Chiba University, 1-33, Yayoicho Inage-ku, Chiba, 263-8522, Japan; Earthquake Research Institute, University of Tokyo, 1-1-1 Yayoi, Bunkyo-ku, Tokyo, 113-0032, Japan; National Research Institute for Earth Science and Disaster Prevention, 3-1 Tennodai, Tsukuba, Ibaraki 305-0006, Japan; Japan Agency for Marine-Earth Science and Technology, 25-3173 Showamachi, Kanazawa-ku, Yokohama, 236-0001, Japan; Graduate School of Science, Tohoku University, 6-6 Aramaki Aza Aoba, Sendai, Miyagi 980-8578, Japan
推荐引用方式 GB/T 7714	Kono A.,Sato T.,Shinohara M.,et al. 2D spatial distribution of reflection intensity on the upper surface of the Philippine Sea plate off the Boso Peninsula, Japan[J],2020,774.
APA	Kono A..,Sato T..,Shinohara M..,Mochizuki K..,Yamada T..,...&Azuma R..(2020).2D spatial distribution of reflection intensity on the upper surface of the Philippine Sea plate off the Boso Peninsula, Japan.Tectonophysics,774.
MLA	Kono A.,et al."2D spatial distribution of reflection intensity on the upper surface of the Philippine Sea plate off the Boso Peninsula, Japan".Tectonophysics 774(2020).