지구물리와물리탐사 (Geophysics and Geophysical Exploration)

  • 제16권4호
  • /
  • Pages.293-299
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  • 2013
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  • 1229-1064(pISSN)
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  • 2384-051X(eISSN)
한국지구물리·물리탐사학회 (Korean Society of Earth and Exploration Geophysicists)
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진원 깊이를 고려한 한반도 다중지연시간창 해석

Multiple Lapse Time Window Analysis of the Korean Peninsula Considering Focal Depth

  • Chung, Tae Woong (Department of Energy & Mineral Resources Engineering, Sejong University) ;
  • Rachman, Asep Nur (Department of Energy & Mineral Resources Engineering, Sejong University)
  • 투고 : 2013.09.16
  • 심사 : 2013.11.18
  • 발행 : 2013.11.30
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초록

최근 한반도의 Direct Simulation Monte Carlo (DSMC)법에 의한 다중지연시간창(Multiple Lapse Time Window; MLTW)법 해석에서 속도구조보다 진원 깊이의 영향이 훨씬 더 크다는 것이 보고되어, 깊이가 약 10 km에 해당되는 지진 41개와 79 지점의 관측점을 잇는 경로가 330개에 이르는 자료에 대하여 DSMC법을 이용, 이전에 연구된 5가지 속도구조를 재검증하였다. 그 결과, 표층 진원을 가정한 해석적 모델보다 10 km 진원의 DSMC법 적용 균일모델의 잔차가 크게 개선된 반면, 속도구조 모델 간의 잔차값 차이는 비교적 작음을 확인하였다.

The recent Multiple Lapse Time Window (MLTW) analysis of Korean Peninsula event showed that the focal depth was far greater influence factor than the velocity structure of the model, applying the analysis of the direct simulation Monte Carlo (DSMC) method. Thus, using the events with focal depth of about 10 km, this study considered 330 paths connecting 41 events and 71 stations, and re-examined uniform and depth-dependent velocity models previously studied. As a result, the residual of misfit function greatly decrease from analytic model to DSMC model, reflecting variation of the focal depth from 0 to 10 km. On the other hand, the difference of residuals for each velocity model were relatively small.

키워드

참고문헌

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