Japan Geoscience Union Meeting 2025

Presentation information

[J] Oral

S (Solid Earth Sciences ) » S-SS Seismology

[S-SS14] Active faults and paleoseismology

Mon. May 26, 2025 1:45 PM - 3:15 PM Exhibition Hall Special Setting (6) (Exhibition Hall 7&8, Makuhari Messe)

convener:Mamoru Koarai(Earth Science course, College of Science, Ibaraki University), Suguru Yabe(National Institute of Advanced Industrial Science and Technology), Kiyokazu Oohashi(National Institute of Advanced Industrial Science and Technology ), Kyoko Kagohara(Yamaguchi University), Chairperson:Mamoru Koarai(Earth Science course, College of Science, Ibaraki University), Suguru Yabe(National Institute of Advanced Industrial Science and Technology)

2:30 PM - 2:45 PM

[SSS14-16] Evaluation of past multi-segment earthquakes on the Median Tectonic Line active fault zone – Vertical displacement history around the pull-apart basin –

*Hisao Kondo1, Haruo Kimura2, Hiroyuki Tsutsumi3, Hideki Kurosawa4 (1.Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, 2.CRIEPI, 3.Doshisha University, 4.Oyo Corporation)

Keywords:Active fault, Paleoseismology, MTL active fault zone, Historical earthquake

The Median Tectonic Line active fault zone (MTL) is the longest strike-slip fault system in Japan, extending from the west of Beppu Bay to the Kii Peninsula for a total length of ca. 444 km (e.g., Okada, 2020; Goto and Nakata, 1998; Earthquake Research Promotion Headquarters Earthquake Investigation Committee, 2017). We have conduct commissioned research projects on the MTL in FY2020-2022 and FY2023-2025 to improve the evaluation method of multi-segment earthquakes caused by long active fault zones. During the past project on the Itoigawa-Shizuoka Tectonic Line Zone, the frequency of past multi-segment earthquakes was estimated from the displacement history, such as past co-seismic displacement per event and precise timing of paleo-earthquakes, and a method was developed to evaluate the occurrence probability of multi-segment earthquakes based on the Poisson process (MEXT and AIST, 2020; Kondo, 2023). On the MTL, mainly on the Shikoku island active fault and paleoseismological surveys are ongoing with the aim of further improving the field survey methods for restoring the co-seismic displacement specific to strike-slip faults and the methods for identifying past multi-segment earthquakes. In this presentation, we will introduce the results of a survey conducted near the segment boundary between the Kawakami fault and the Okamura Fault, where a pull apart basin was formed due to right step of those right-lateral strike-slip faults.

Acknowledgement: This research was partly conducted under the research project "Research project on improving evaluation methods for multi-segment earthquakes produced by long active fault zones" by MEXT. We would like to express our gratitude to all involved.