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Crustal-scale fault systems in the Korean Peninsula unraveled by reflection seismic data
  • +8
  • Samuel Zappalá,
  • Alireza Malehmir,
  • Tae-Kyung Hong,
  • Christopher Juhlin,
  • Junhyung Lee,
  • Myrto Papadopoulou,
  • Bojan Brodic,
  • Seongjun Park,
  • Dongchan Chung,
  • Byeongwoo Kim,
  • Jeong-in Lee
Samuel Zappalá
Uppsala University

Corresponding Author:[email protected]

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Alireza Malehmir
Uppsala University
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Tae-Kyung Hong
Yonsei University
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Christopher Juhlin
Uppsala University
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Junhyung Lee
Yonsei University
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Myrto Papadopoulou
Uppsala University
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Bojan Brodic
Uppsala University
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Seongjun Park
Yonsei University
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Dongchan Chung
Yonsei University
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Byeongwoo Kim
Yonsei University
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Jeong-in Lee
Yonsei University
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Abstract

An approximately 40-km long high-resolution reflection seismic profile (P3) was acquired in the metropolitan area of Seoul in South Korea for the purpose of fault system imaging in a highly noisy and challenging urban environment. Two 12t seismic vibrators (mini-vibs) were used as the seismic source. Data were recorded using a dual element seismic spread; 20 m spaced 421 wireless seismic recorders connected to 10 Hz geophones and 20 micro-electro-mechanical (MEMS-based) landstreamer sensors (2 m sensor spacing) attached to one of the vibrators. The purpose of the dual spread employed was to delineate both near-surface and deep structures. The processing results show good quality and the processing work was complemented by different analysis to further constraints the geological interpretation. The survey results provide evidence for the 3D geometry of three fault systems, including Chugaryeong, Pocheon and Wangsukcheon faults. A gently westerly-dipping set of reflectivity underlying a domed-shaped package of reflectivity is interpreted as a fault, and could project to the known surface position of the Pocheon fault. The domed-shaped reflectivity is interpreted as folded and faulted dyke or sill systems. Downward continuation of the interpreted fault intersects the sub-vertical Chugaryeong fault in a zone where the current seismicity is observed, suggesting that these two major fault systems may have jointly evolved in the form of splay faults. Reflections from the Wangsukcheon fault are also present in the data and interpreted to dip approximately 60 degrees to the east, in an opposite direction to the two other faults.