Horizontal sliding of kilometre-scale hot spring area during the 2016 Kumamoto earthquake

Takeshi Tsuji, Jun'Ichiro Ishibashi, Kazuya Ishitsuka, Ryuichi Kamata

Research output: Contribution to journalArticlepeer-review

16 Citations (Scopus)

Abstract

We report horizontal sliding of the kilometre-scale geologic block under the Aso hot springs (Uchinomaki area) caused by vibrations from the 2016 Kumamoto earthquake (Mw 7.0). Direct borehole observations demonstrate the sliding along the horizontal geological formation at ∼50 m depth, which is where the shallowest hydrothermal reservoir developed. Owing to >1 m northwest movement of the geologic block, as shown by differential interferometric synthetic aperture radar (DInSAR), extensional open fissures were generated at the southeastern edge of the horizontal sliding block, and compressional deformation and spontaneous fluid emission from wells were observed at the northwestern edge of the block. The temporal and spatial variation of the hot spring supply during the earthquake can be explained by the horizontal sliding and borehole failures. Because there was no strain accumulation around the hot spring area prior to the earthquake and gravitational instability could be ignored, the horizontal sliding along the low-frictional formation was likely caused by seismic forces from the remote earthquake. The insights derived from our field-scale observations may assist further research into geologic block sliding in horizontal geological formations.

Original languageEnglish
Article number42947
JournalScientific reports
Volume7
DOIs
Publication statusPublished - Feb 20 2017

All Science Journal Classification (ASJC) codes

  • General

Fingerprint Dive into the research topics of 'Horizontal sliding of kilometre-scale hot spring area during the 2016 Kumamoto earthquake'. Together they form a unique fingerprint.

Cite this