• Title/Summary/Keyword: 진앙거리

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A study of $Q_{Lg}^{-1}$ by the reversed two station method in the crust of central South Korea (Reversed Two Station Method (RSTM)에 의한 중부지방 $Q_{Lg}^{-1}$ 연구)

  • Cheong, Tae-Woong
    • Journal of the Korean Geophysical Society
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    • v.5 no.3
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    • pp.211-218
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    • 2002
  • The reversed two station method (RSTM) devised by Chun et al. (1987) is widely used to obtain $Q_{Lg}^{-1}$ for Lg wave data with hypocentral distance greater than 90 km. By applying RSTM to the Lg data of central South Korea with hypocentral distance between 95 and 381 km, we obtained high $Q_{Lg}^{-1}$. The value of $Q_{Lg}^{-1}$ is very similar with that of southeastern S. Korea, which is derived from the same method for similar distances. The studied hypocentral range seems to distort $Q_{Lg}^{-1}$ to high value because decay rate in this range is higher than 0.5, which is typical decay rate of surface wave.

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확률론적 지진위험도의 불확실성 영향인자의 단계별 범위 영향 분석

  • 김준경;윤철호;이성규;임창복;김문수
    • Proceedings of the Korean Nuclear Society Conference
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    • 1996.05d
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    • pp.405-409
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    • 1996
  • 본 연구는 일정 지역의 확률론적 지진위험도 (Probabilistic Seismic Hazard) 평가와 관련하여 전문가가 제시한 제1차 입력자료를 이용하여 제2차 입력자료를 도출할 때 입력자료의 다단계화를 통하여 각 단계별 구간의 입력자료가 확률론적 지진위험도 불확실성에 미치는 상대적 영향을 분석하였다. 확률론적 지진위험도 분석을 위하여 미국지질조사연구소 (USGS) 및 미국 로렌스리버모어 연구소(LLNL)가 개발한 전산코드를 각각 이용하였고 또한 전문가가 제시한 제 1차 입력자료는 기존 연구보고서에서 주어진 자료를 이용하였다. 분석결과 지진활동도 변수 특히 지진규모의 각 단계 및 감쇠특성함수의 진앙거리 단계에 따라서 확률론적 지진위험도의 절대값 및 불확실성에 미치는 영향의 차이가 상대적으로 크다는 것이 확인되었다. 또한 부지별로 이러한 분석을 함으로서 확률론적 지진 위험도 곡선에 영향을 미치는 임의 부지에 고유한 임계 지진규모 및 임계 진앙거리에 대한 분석을 통하여 전반적으로 불확실성을 감소시킬 수 있다.

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Characteristic Investigation of the Bedrock Earthquake Records for the Structural Time-History Seismic Analyses (구조물의 시간이력 지진해석을 위한 암반지진기록의 특성분석)

  • Kim, Yong-Seok
    • Journal of the Earthquake Engineering Society of Korea
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    • v.12 no.1
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    • pp.89-95
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    • 2008
  • Until recently lots of time-history seismic analyses were performed with the earthquake motions recorded at the soft soil surface without taking into account the effects of the soft soil amplification. However, it is important to utilize the bedrock seismic motions for the rational seismic analyses of a structure considering the site soil conditions. In this study, 26 bedrock earthquake records were selected from publicly available 1557 seismic records provided by the Pacific Earthquake Engineering Research Center (PEER) for the study, and the characteristics of them were investigated. Study results showed that it is not reasonable to estimate earthquake acceleration intensity from the magnitude of an earthquake without considering the site soil conditions and it is also hard to draw any general relationships between earthquake acceleration intensity, earthquake magnitude and epicenter distance with bedrock earthquake records in the PEER database. However, 26 bedrock earthquake records selected in this study can be utilized for the time-history seismic analyses of a structure-soil system as bedrock earthquake ones, and it is also confirmed that it is necessary to take into account acceleration intensity, magnitude, epicenter distance and site conditions simultaneously for the proper use of those selected earthquake records.

Characteristics of Vertical/Horizontal Ratio of Response Spectrum from Domestic Ground Motions (국내 관측자료를 이용한 응답스펙트럼의 수직/수평비 특성 분석)

  • Kim, Junkyoung
    • Journal of the Korean GEO-environmental Society
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    • v.12 no.1
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    • pp.81-87
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    • 2011
  • The characteristics of vertical to horizontal ratio of response spectrum from 20 recent earthquakes were analysed. Response spectrum of 260 horizontal and 130 vertical ground motions were normalized by peak ground acceleration at each resonance frequency from 0.1 to 50Hz. It has been identified that the ratio of vertical to horizontal response spectrum has strong dependancy on epicentral distance and resonance frequency. The ratio of vertical to horizontal response spectrum for the 0-50km epicentral distance group are larger than 2/3 values, which is a standard engineering rule-of-thumb V/H=2/3, at resonance frequency above 7-8Hz. All the 3 groups such as 50-100, 100-150- and 150-200km epicentral distance have shown larger values of vertical to horizontal ratio than 2/3 at resonance frequency above 15Hz and also are larger than 2/3 at resonance frequency below 8-10Hz. Even though there are differences in specific resonance frequency values which depend on the epicentral distance group, we should be careful of seismic design of vertical component of the structures winch are located within the range of about 200km distance. form the potentially seismic causative faults.

Intensity Attenuation in the Sino-Korea Craton (Sino-Korean 지괴에서의 진도감쇠)

  • 이기화
    • Proceedings of the Earthquake Engineering Society of Korea Conference
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    • 1999.04a
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    • pp.27-31
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    • 1999
  • 진도의 거리에 따른 감쇠양상은 두가치 측면에서 중요하다. 첫째는 역사지진의 크기를 평가하는데 사용되고 둘째는 역사지진자료를 이용하여 지진위험도를 평가하는데 이용된다. 한반도의 경우 대부분의 지진활동 자료가 역사지진이므로 이지진들의 크기를 결정하고 이들을 이용하여 지진위험도를 평가하기 위하여 합리적인 진도감쇠양상의 결정은 매우 중요한 과제라 할수 있다 진도의 감쇠양상은 진앙진도와 진앙거리 등 두요소에 같이 의존함이 알려져 있으므로 한반도에서 MMI VIII만의 지진자료를 이용하여 결정된 Lee의 기존의 감쇠공식은 그 사용범위에 한계가 불가피하므로 상기 두 가지 요소를 함께 고려한 새로운 감쇠공식의 유도가 요구되어진다. 지체구조적으로 Sino-Korean 지괴라고 불리우는 중국 북동부와 한반도에서 발생한 MMI VIII-X 지진들의 자료를 이용하여 한반도에서 발생하는 MMI VIII-X의 강진들에 대한 새로운 진도감쇠양상을 결정하였다.

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Detection and Analysis of the Artificial Underground Explosions in N. Korea using KSRS data. (KSRS 자료를 이용해서 북한의 인공지하폭발의 탐지 및 분석)

  • 김소구;이승규;마상윤;박용철
    • The Journal of Engineering Geology
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    • v.5 no.2
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    • pp.181-192
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    • 1995
  • The discrimination studies between earthquakes and underground nuclear explosions have been carried out by various seismologists(Nuttli and Kim, 1976; Dahiman and Israelson, 1977; Masse, 1981). The discrimination between local microearthquakes and artificial underground explosions(epicentral distance not greater than 400Km), however, has not been actively studied so far in the light of seismological aspects. Futhermore this kind of research has never been performed in Korea even if it is of great importance for IAEA (International Atomic Energy Agency) to clearly analyze the military nuclear power of North Korea at present. This research has been carried out by using some of the artificial underground explosions(about 100 events) have occurred in North Korea for the last six years. The azimuths, apparent incidence angles, epicentral distances and locations are determined using a single station of 3 - component data. The detection, location and identification are performed through the polarization and the bandpass filtering. This technique can be also applied to study the inhomogeneous crustal structure finding the converted waves.

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Estmation of Magnitude of Historical Earthquakes Considering Earthquake Characteristics and Aging of a House (지진특성 및 가옥의 노후도를 고려한 역사지진의 지진규모 추정)

  • 서정문;최인길
    • Journal of the Earthquake Engineering Society of Korea
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    • v.2 no.4
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    • pp.1-10
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    • 1998
  • The magnitudes of historical earthquake records related with house collapses are estimated considering the magnitude, epicentral distance, soil condition and aging of a house. Eighteen artificial time histories for magnitudes 6-8, epicentral distances 5 km-350 km and hard and soft soil condition were generated. Nonlinear dynamic analyses were performed for a traditional three-bay-straw-roof house. The aging effect of the house was modeled as such that the lateral loading capacity of wooden frames represented by hysteretic stiffness was decreased linearly with time. The house was idealized by one degree-of-freedom lumped mass model and the nonlinear characteristics of wooden frames were modeled by the Modified Double-Target mode. For far field earthquakes, minor damages were identified regardless of magnitude, soil condition and aging of the house. For intermediate field earthquake, earthquake magnitude greater than 6.5 caused severe damages in soil sites. For near field earthquake, severe damages occurred for magnitude greater than 6.5 regardless of soil condition and aging of the house. It is estimated that the magnitude of historical earthquakes is about 6.2. An empirical equation of magnitude-intensity relationship suitable to Korea is suggested.

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Earthquake-related Data Selection using Event Packets (이벤트 패킷을 이용한 지진관련 데이터의 추출)

  • Lim, In-Seub;Jung, Soon-Key
    • Journal of the Korea Society of Computer and Information
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    • v.13 no.6
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    • pp.59-68
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    • 2008
  • In this paper, we propose a method for selecting meaningful event packets from which can receive before anything else from seismograph according to allotted priority and estimate epicenter using selected packets. Event packets which received from each station will be evaluated with their onset time, signal period and SNR by statistical method and will be selected packets related with real earthquake's P-wave. And estimated epicenters using by 'Application of epicenter estimation using first P arrivals'. With local earthquakes occurred in 2007 were announced by KMA, collected event packets on earthquake happened date and selected p-wave related packets and estimated epicenter. After result of experiment, if an earthquake occurred within seismic networks, can estimate epicenter with small misfits just after event packets arrived from above 4 stations. Considering average distance of each station, in case of using all stations' data include other organization, can estimate and alert rapidly. It show this method is useful when construct a local earthquake early warning system later.

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Hypocentral Depth Determination of Gyeongju Earthquake Aftershock Sequence (경주 지진 여진의 진원 깊이 연구)

  • Chung, Tae Woong;Iqbal, Muhammad Zafar
    • Geophysics and Geophysical Exploration
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    • v.20 no.1
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    • pp.49-55
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    • 2017
  • Hypocentral depths of 103 aftershocks of the 12 September 2016 Gyeongju earthquake (ML 5.8) were inverted by epicentral relocation, using HYPO71 and HYPOINVERSE. From the comparison of seven models that reflect regional velocity structure in the southern Korean Peninsula, HYPO71 with linear weighting over the whole range showed less residuals than HYPOINVERSE for the model near the epicenter. Less uncertainties of focal depths were observed for the events with large magnitude and short range of the closest S-phase distance.

Estimation of epicenter using an empirical relationship between epicentral distance and traveltime of the first arrival (초동 전파시간과 진앙거리의 경험적인 관계를 이용한 진앙 추정)

  • Sheen, Dong-Hoon;Baag, Chang-Eob;Hwang, Eui-Hong;Jeon, Young-Soo
    • 한국지구물리탐사학회:학술대회논문집
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    • 2007.06a
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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.

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