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10 years after the 2011 Tohoku earthquake: A milestone of solid earth science

Progress in Earth and Planetary Science welcomes submissions to the special issue on '10 years after the 2011 Tohoku earthquake: A milestone of solid earth science'.
 

A number of new discoveries have been made in the aftermath of the 2011 Tohoku earthquake, thanks to unprecedented near-field observations as well as to the earth scientific knowledge about the northeastern Japan arc that has accumulated prior to the earthquake.  The earthquake highlighted the complexity of frictional behaviors on the shallowest part of the subduction interface, previously regarded as mostly aseismic. Several pieces of evidence have been presented that illuminate the spatial correlation between the distribution of interplate faulting events of various sizes and time scales and associated structural heterogeneities. The stress re-distribution processes after the earthquake, including viscoelastic deformation and fluid remobilization, have been revealed both in the overriding and incoming plates and provide new insights in the dynamics of the subduction zone. Abundant records of the associated tsunami clarified various processes during the generation, propagation, and inundation of tsunamis. The earthquake also provides a unique opportunity to compare the fault model constrained by modern observations with those of past earthquakes based on geological records so that we can improve the reconstructed recurrence history of massive earthquakes. It is expected that a collection of research contributions regarding the Tohoku earthquake will benefit our general understanding regarding infrequent great (M > 9) subduction earthquakes.

In this special issue of SPEPS, we invite authors to contribute their latest research or reviews on the seismotectonics along the northeastern Japan margin from disciplinary and interdisciplinary viewpoints. The scope of this issue ranges across, but is not limited to, the diversity of fault behaviors along the plate boundary and its relation to structural heterogeneity of the plate boundary zone, postseismic deformation and seismicity, behavior of tsunamis, and earthquake geology and paleoseismology along the Japan trench.


Deadline for submissions

Submission start: 1 October 2021

Submission deadline:  31 August 2022

Guest Editors

Takeshi Iinuma
JAMSTEC
email: iinuma@jamstec.go.jp

Shuichi Kodaira
JAMSTEC
email: kodaira@jamstec.go.jp

Masaki Yamada
Shinshu University
email:  yamada@shinshu-u.ac.jp

Roland Bürgmann
University of California, Berkeley
email: burgmann@seismo.berkeley.edu

Toru Matsuzawa
Tohoku University, Japan
email: toru.matsuzawa.c6@tohoku.ac.jp

Ryota Hino
Tohoku University, Japan
email: hino@tohoku.ac.jp

  1. Slow earthquakes are episodic slow fault slips. They form a fundamental component of interplate deformation processes, along with fast, regular earthquakes. Recent seismological and geodetic observations have ...

    Authors: Tomoaki Nishikawa, Satoshi Ide and Takuya Nishimura
    Citation: Progress in Earth and Planetary Science 2023 10:1
  2. Long-term continuous observation of seafloor pressure is effective for detecting seafloor vertical deformations that are associated with transient tectonic phenomena such as slow slip events. Since the aseismi...

    Authors: Ryota Hino, Tatsuya Kubota, Naotaka Y. Chikasada, Yusaku Ohta and Hideto Otsuka
    Citation: Progress in Earth and Planetary Science 2022 9:73
  3. Paleotsunami deposit investigations and numerical tsunami computations have been performed to elucidate the source and size of large tsunamis along the Kuril to Japan Trenches, particularly for unusual tsunami...

    Authors: Kai Sato, Masaki Yamada, Daisuke Ishimura, Takashi Ishizawa and Toshitaka Baba
    Citation: Progress in Earth and Planetary Science 2022 9:72
  4. A decade after the 2011 Tohoku-oki earthquake (Mw 9.0), geological surveys were conducted at multiple sites along the Pacific Coast of the tsunami-inundated Tohoku region in Japan, providing thousands of years...

    Authors: Daisuke Ishimura, Takashi Ishizawa, Masaki Yamada, Kaori Aoki and Kai Sato
    Citation: Progress in Earth and Planetary Science 2022 9:69
  5. Temporal seismic observations from pop-up type ocean-bottom seismometers were used to detect tectonic tremors immediately following the 2011 Tohoku-Oki earthquake in the northern periphery of the aftershock ar...

    Authors: Hidenobu Takahashi, Ryota Hino, Naoki Uchida, Takanori Matsuzawa, Yusaku Ohta, Syuichi Suzuki and Masanao Shinohara
    Citation: Progress in Earth and Planetary Science 2022 9:66
  6. The 2011 Tohoku-Oki earthquake generated a surprisingly large near-trench slip, and earth scientists have devoted significant attention to understanding why. Some studies proposed special rupture mechanisms, s...

    Authors: Tatsuya Kubota, Tatsuhiko Saito and Ryota Hino
    Citation: Progress in Earth and Planetary Science 2022 9:68
  7. A quantitative understanding of paleotsunamis is a significant issue in tsunami sedimentology. Onshore tsunami deposits, which are geological records of tsunami inundation, are used to reconstruct paleotsunami...

    Authors: Hidetoshi Masuda, Daisuke Sugawara, Tomoya Abe and Kazuhisa Goto
    Citation: Progress in Earth and Planetary Science 2022 9:65
  8. The transition process from coseismic to early postseismic phenomena within a half-day remains a significant topic for understanding the slip budget and friction properties of the fault. However, the investiga...

    Authors: Yusuke Tanaka, Yusaku Ohta and Shin’ichi Miyazaki
    Citation: Progress in Earth and Planetary Science 2022 9:55
  9. The distributions of sandy tsunami deposits do not reflect the true extents of tsunami inundation areas, leading to underestimates of inundation by past tsunamis and thus the magnitudes of their associated tsu...

    Authors: Tetsuya Shinozaki, Yuki Sawai, Minoru Ikehara, Dan Matsumoto, Yumi Shimada, Koichiro Tanigawa and Toru Tamura
    Citation: Progress in Earth and Planetary Science 2022 9:29