Journal of the Korean Geophysical Society (지구물리)

Korean Society of Earth and Exploration Geophysicists (한국지구물리·물리탐사학회)
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Electrical resistivity and seismic reflection mapping for the southeastern part of the Yongdong basin (Cretaceous), Korea

영동분지(백악기) 남동부의 전기비저항 및 탄성파탐사자료 해석

  • Kim, Ji-Su (Department of Earth and Environmental Sciences, Chungbuk University) ;
  • Han, Su-Hyeong (Department of Earth and Environmental Sciences, Chungbuk University) ;
  • Lee, Cheol-U (Department of Earth and Environmental Sciences, Chungbuk University) ;
  • Kim, Bok-Cheol (Petroleum and Marine Division, Korea Institute of Geology, Mining and Materials) ;
  • Yang, U-Heon (Petroleum and Marine Division, Korea Institute of Geology, Mining and Materials) ;
  • Son, Ho-Ung (Department of Geotechnical and Environmental Engineering, Paichai University) ;
  • Son, Yeong-Gwan (Department of Earth and Environmenatl Sciences, Gyeongsang University)
  • Published : 20000600
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Abstract

Five electrical resistivity dipole-dipole and two seismic reflection surveys were performed in the southeastern margin of the Yongdong basin to delineate the shallow basin architecture. To investigate the intra-basin structure, twenty four resistivity sounding points and three dipole-dipole lines were selected especially in the vicinity of volcanic masses. The basin-fault boundaries are identified in electrical dipole-dipole resistivity section as high resistivity-contrast of approximately $1,500\;{\Omega}{\cdot}m$, characterized as a band of high standard-deviation. They are also effectively clarified in the seismic reflection data: amplitude and continuity contrasts in the common shot gather, first-arrival profiles, complex attribute plots. The intra-basin resistivity structures are constructed by interpolating vertical electrical sounding data and dipole-dipole profiles. The high-resistivity anomalies most likely originate from the northsouth-trending and northeast-dipping volcanic masses, which are to be further quantitatively investigated with geomagnetic and magnetotelluric surveys.

영동분지(백악기) 남동부 지역의 천부 구조를 파악하기 위하여 분지의 경계 부근에서 5 개 측선의 전기비저항 쌍극자탐사와 2 개 측선의 탄성파 반사법탐사를 수행하였다. 또한 분지 안에 존재하는 화산암체 부근에서 총 24 점의 전기비저항 수직탐사와 3 개의 쌍극자탐사를 실시하였다. 분지 경계에 대한 전기비저항값은 쌍극자단면도에서 예상 단층선을 기준으로 약 $1,500\;{\Omega}{\cdot}m$의 대비를 보이며 표준편차 또한 경계 부근에서 가장 크게 나타난다. 분지의 경계 단층은 탄성파 공통발파점자료에서 진폭 대비, 이벤트의 연속성 대비, 초동의 기울기 차이, 복소트레이스 단면도의 특성에 의해 효과적으로 확인되었다. 분지 안의 전기비저항 구조는 쌍극자탐사 및 전기비저항 수직탐사자료 해석 결과 북동방향의 고비저항대가 단속적으로 나타나고 있는데 이것은 남북방향으로 분포하는 북동방향의 경사를 가진 화산암체에 의한 반응으로 해석된다. 이에 대한 자세한 해석을 위해서는 앞으로 자력 및 자기지전류 탐사가 추가로 수행되어야할 것이다.

Keywords

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