• 지구물리
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• 제3권4호
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• pp.261-268
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• 2000

기상청 지진목록에 대하여 지진활동 매개변수 추정을 위한 최소규모를 분석하였다. 한반도 남부지역 전체에 대하여, 규모별 발생빈도의 시간적 변화로부터 규모 3.0이 적절한 최소규모로 추정되었다. 최소규모 3.0이상 지진의 발생빈도로부터 추정된 b 값은 1.11로서 이전의 연구결과에 비하여 크게 나타났다. 한반도 남부지역을 $0.1^{\circ}{\times}0.1^{\circ}$ 격자로 나누어 최소규모의 공간적 분포를 분석한 결과 많은 지점에서 최소규모에 대한 통계적 기준을 만족시키지 못하는 것으로 나타났다. 통계적 기준을 만족하는 지점은 주로 동부지역에 집중되며, 이 지역에서 최소규모는 $2.4{\sim}3.5$이다. 또한 b 값은 $0.75{\sim}1.73$ 이며, 평균은 1.08로서 한반도 남부지역 전체에 대한 값과 유사하다.

• 한국지진공학회:학술대회논문집
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• 한국지진공학회 2002년도 추계 학술발표회 논문집
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• pp.28-34
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• 2002

The b-value in the magnitude-frequency relationship logN(m) = $\alpha$ - bmwhere N(m) is the number of earthquakes exceeding magnitude m, is important seismicity parameter In hazard analysis. Estimation of the b-value for earthquake data observed on KSRS array network is done employing the maximum likelihood technique. Assuming the whole Korea Peninsula as a single seismic source area, the b-value is computed at 0.9. The estimation for KMA earthquake data is also similar to that. Since estimate is a function of minimum magnitude, we can inspect the completeness of earthquake catalog in the fitting process of b-value. KSRS and KMA data lists are probably incomplete for magnitudes less than 2.0 and 3.0, respectively. Examples from probabilistic seismic hazard assessment calculated for a range of b-value show that the small change of b-value has seriously effect on the prediction of ground motion.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2007년도 공동학술대회 논문집
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• pp.64-68
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• 2007

The classic graphical method to determine the epicenter uses differences between the arrival times of P and S waves at each station. In this research, a robust approach is proposed, which provides a fast and intuitive estimation of earthquake epicenters. This method uses an empirical relationship between epicentral distance and traveltime of the first arrival P phase of local or regional earthquake. The relationship enables us to estimate epicentral distances and draw epicentral circles from each station with P-traveltimes counted from a probable origin time. As the assigned time is getting close to the origin time of the earthquake, epicentral circles begin to intersect each other at a possible location of the epicenter. Then the possibility of the epicenter can be expressed by a function of the time and the space. We choose the location which gives the minimum standard deviation of the origin time as an estimated epicenter. In this research, 918 P arrival times from 84 events occurring from 2005 to 2006 listed in the KMA earthquake catalog are used to determine the empirical P-traveltime function of epicentral distances.