Active faults in Korea - Tohoku University Official...
Transcript of Active faults in Korea - Tohoku University Official...
Choi, Jin-HyuckActive Tectonics Research Team, KIGAM
email: [email protected]: https://sites.google.com/site/jinhyuckchoi9521/
Active faults in Korea: recent research & current trends
Collaboration withKim, Y.-S. et al (Korean Active Fault Research Group)Lee, S.-R. et al (KIGAM project_17-3112)
CCOP-IUGS Task Group on Geohazards (TGG) Joint Seminar 30 Oct. 2018
MW 5.5 GJ eq. (Sep. 2016)
MW 5.4 PH eq. (Nov. 2017)
We are here
(updated from Roger Bilham, 2009)
Large earthquakes cause destructive disaster
1906 Mw 7.8 San Francisco eq. along the San Andreas fault
Earthquake rupture for all individual events
Earthquake ‘surface’ rupture for seismic events larger than MW 5.5
(Single-fault magnitude frequency relation) (Down-dip rupture width of earthquakes)
Surface records of large earthquakes
(Zielke & Arrowsmith, 2008)
Plate tectonic setting & Crustal deformation
- No large (M ≥ 5.5) earthquake in South Korea (1900 - early 2016)
- Unobservable crustal (fault) deformation (except for the 2011 Tohoku-Oki ep.)
(USGS) (Absolute velocities before(red) and after(blue) the 2011 Tohoku-Oki eq.: Kim et al.., 2015)
We are here
Historical & Instrumental seismicity
(KMA)
MMI > V (2-1904) 2 ≤ M ≤ 5.5 (1978-2017)
- 15 large historical earthquakes (the estimated magnitude: 6.5 < ML < 6.9)
- 10 moderate-sized (5 ≤ M ≤ 5.5) instrumental earthquakes
2017 Mw 5.42016 Mw 5.5
Active faults - Large (M ≥ 5.5) earthquakes during the Quaternary
Wangsan Fault(from Choi, W.-H.’s presentation)
YSD
YSDUC
UC
Andesite
Andesite
- Stratigraphic records data at ~ 100 sites
- No published active fault map
- Long recurrence interval of large eqs.
- We are living in long inter-seismic period
No surface rupture
ALOS-2 PALSAR images(21/07/2015 & 13/09/2016)
The 2016 MW 5.5 Gyeongju earthquake
(Elliott et al., 2016) (Kim et al., 2017)Next slide
Flow diagram of post-earthquake research No surface rupture, but aftershock sequence
(Kim et al., 2017)
Earthquake rupture on a subsidiary fault in western damage zone of the Yangsan Fault
(Central Geological Survey, Taiwan)
- Active fault map for the entire area of S. Korea
(KAFRG, 2017-2036)
- Strip map of the Central Yangsan Fault
(the epicenter area of the 2016 Gyeongju eq.)
(KIGAM, 2017-2019)
Active faults project (after the 2016 MW 5.5 Gyeongju eq.)
Development of investigation and evaluation technology for active faults in Korea
Private Advisory Board National Institute for Disaster Prevention
Main research institutePKNU
• Standardization
• Topographic analysis
• Structure analysis
• Paleoseismological
analysis
Joint research instituteKIGAM
Joint research instituteKBSI
Joint research institutePNU
Ministry of the Interior and Safety
• Topographic analysis
• Structure analysis
• Paleoseismological
analysis
• Topographic analysis
• Structure analysis
• Paleoseismological
analysis
• Development of
analysis protocol
• Dating
• Dating data verification
Committedresearch institutionChung-Ang Aero Survey
• Imaging LiDAR image
Committed research institutionSaehan Aero Survey
• Imaging LiDAR image
KAFRG (Korean Active Fault Research Group, 2017-2036)
(Haddad et al., 2012)(Howle et al., 2012)
Airborne LiDAR
Active faults project - The southern sections of the Yangsan Fault (YSF)
100 m
- Wallace Creek along the San Andreas Fault
(Sieh and Jahns, 1984; Sieh and Wallace, 1987)
Abandoned channel
Smaller horizontal displacement
along the central (?) Yangsan Fault
- Younger geomorphic marker ? - Lower slip-rate ? - Longer recurrence time ?- More distributed deformation ?
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Fault Segmentation
(Wesnousky, 2006)
(Mignan et al., 2015)
- Earthquake rupture propagation is directly affected by the fault geometry and discontinuities
- Fault segmentation is an essential factor to define earthquake cycle models
Segmentation of the Yangsan Fault
Along-fault variations in geologic inheritance, geomorphic features, fault geometry, and seismic patterns
The 2017 MW 5.4 Pohang earthquake
No surface rupture, but second-order surface deformations (Choi et al., in press)
(Lee et al., 2014)(Choi et al., in press)
Surface evidence of paleo-earthquakes
Summary
- Recent two moderate-sized earthquakes occurred in the
southeastern part of the Korean Peninsula.
- There have been multiple large (M ≥ 5.5) earthquakes along
the Yangsan Fault and on its eastern block, and there are
neotectonically active crustal structures in this region.
- Geomorphic expression of the fault, which is observable in
high-resolution topographic data, plays a key role in the study
of paleo-earthquakes.
- It is needed to date more offset geomorphic markers (slip-rate)
and to excavate ‘young’ but ‘old’ stratigraphic records (temporal
history).