Assessing whether the 2017 M w 5.4 Pohang earthquake in South Korea was an induced event

Author:

Kim Kwang-Hee1ORCID,Ree Jin-Han2ORCID,Kim YoungHee3ORCID,Kim Sungshil2ORCID,Kang Su Young1ORCID,Seo Wooseok1ORCID

Affiliation:

1. Department of Geological Science, Pusan National University, Busan 46241, Republic of Korea.

2. Department of Earth and Environmental Sciences, Korea University, Seoul 02841, Republic of Korea.

3. School of Earth and Environmental Sciences, Seoul National University, Seoul 08826, Republic of Korea.

Abstract

Triggering quakes in a geothermal space Enhanced geothermal systems (EGSs) provide a potentially clean and abundant energy source. However, two magnitude-5 earthquakes recently occurred in South Korea during EGS site development. Grigoli et al. and Kim et al. present seismic and geophysical evidence that may implicate the second of these earthquakes, which occurred in Pohang, as an induced event. The combination of data from a local seismometer network, well logs, satellite observations, teleseismic waveform analysis, and stress modeling leads to the assessment that the earthquake was probably or almost certainly anthropogenically induced. The possibility remains that the earthquake occurred coincidentally at the EGS site location, but the aftershock distribution and other lines of evidence are concerning for future development of this geothermal resource. Science , this issue p. 1003 , p. 1007

Funder

Korea Foundation of Nuclear Safety (KoFONS) using financial resources granted by the Nuclear Safety and Security Commission (NSSC) of the Republic of Korea

the Korea Meteorological Administration Research Development Program

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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