• Title/Summary/Keyword: 한반도지역

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A Study on Natural Cave developed at Bongye Area in Liaoning Province (요녕성 본계지역 자연동굴 탐사기)

  • Kim, Jung-Hwoi
    • Journal of the Speleological Society of Korea
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    • no.67
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    • pp.73-79
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    • 2005
  • Cave survey is close relate to the culture and environment of the Area. And the Korean culture and the skeleton of the spirits are very similar to that of continent. in this paper some caves are studied and find the close relationship between the present culture and the past cultures.

Evolution of the Subcontinental Lithospheric Mantle of Korean Peninsula: Partial Loss and its Timing (한반도 대륙암권맨틀의 진화: 부분적 손실과 그 시기)

  • Park, Kye-Hun
    • The Journal of the Petrological Society of Korea
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    • v.19 no.3
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    • pp.199-208
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    • 2010
  • The Cenozoic alkali basalts are distributed over Korea, both on central part as Bangnyeongdo, Ganseong, Pyeongtaek-Asan and Jogongni and also on southernmost part Jejudo. The ultramafic mantle xenoliths carried by Korean alkali basalts are spinel lherzolites. Garnet lherzolite that is more stable at the deeper level has not been reported so far, indicating that the lithospheric thickness under Korea does not reach deep enough to the stable zone of garnet lherzolite. The crustal evolution history of the Korean peninsula, at least some part of it, seemingly started since the Archean, it normally should have lithospheric thickness greater than 150 km. However, the mantle xenoliths carried by the Cenozoic alkali basalts indicate the maximum depth of origination in the much shallower range of 60-90 km. Such significantly thinner lithospheric thickness of the Korean peninsula than expected is quite similar to the case of North China Craton having lithospheric thickness of ca. 80 km in average, suggesting thinning of the lithospheric mantle in a depth scale of a few tens of kilometers during the past geologic time. The main causal events for such significant thinning of the lithospheric mantle can be continental collisional events of Paleoproterozoic and early Mesozoic similar to the case of North China Craton, which are also supported by Paleoproterozoic igneous and metamorphic events during the 1.9-2.0 Ga occurring all over the Korean peninsula and also early Mesozoic continental collisional event which has been discussed on lively arguments.

Current State of Stress in South-East Korea (한반도 남동부의 현생 응력장)

  • Lee, Jun-Bok;Chang, Chan-Dong
    • The Journal of Engineering Geology
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    • v.17 no.2 s.52
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    • pp.299-307
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    • 2007
  • We collected data of hydraulic fracturing tests and overcoring tests conducted in 84 boreholes in the south-east Korea in order to analyze the contemporary state of stress in this region. The average direction of the maximum horizontal stress was determined to be $N66^{\circ}{\pm}31^{\circ}E$. The relative magnitudes of the three principal stresses was ${\sigma}_v$ (vertical stress) < ${\sigma}_h$ (minimum horizontal stress) < ${\sigma}_H$ (maximum horizontal stress), indicating thrust fault stress regime. The stress ratio K (horizontal stress/vertical stress) was relatively high (2.2

A Study on the way of Informatization Cooperation in the Korean Peninsula toward the Intelligence Information Society (지능정보사회를 향한 한반도 정보화 협력방안에 관한 연구)

  • Jin, Sang-Ki
    • Informatization Policy
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    • v.27 no.2
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    • pp.84-105
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    • 2020
  • This paper is designed to deal with the gaps and differences between the two Koreas, which have gradually increased since the Korean War. The purpose of this study, in particular, is to assess the digital and AI gap between the two parts of the peninsula in the emerging 4th industrial revolution era that is rapidly innovating the industrial structures, and to present a cooperation plan for the realization of a peace economy and economic prosperity of the Korean Peninsula in the future. In this study, policy alternatives for assessing and bridging the digital gap between South and North were drawn using the comprehensive policy (model) for closing the digital divide, which was one of Korea's past informatization policies. The derived alternatives are meaningful in that they can spark discussions for building the AI-driven society that realizes the integrated economy of the two Koreas complying with the future industrial structure.

Mineralogical characterization of the dust storm in spring of 2002 at Seoul, Korea (2002년 봄 서울지역 황사의 광물특성)

  • 이성록;김기현
    • Proceedings of the Korea Air Pollution Research Association Conference
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    • 2003.05b
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    • pp.409-410
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    • 2003
  • 2002년 봄철 기간 중 한반도지역에서 관측된 황사는 전례를 찾기 어려울 정도로 고농도의 분진량을 기록하였다. 따라서 이 기간 중에는 전국 각지에 산재한 다수의 초등학교가 임시휴교령을 내려야 하였을 정도로 황사현상의 영향이 대단히 심각하였다. 본 연구진은 서울시 북동부 지점의 관측점으로부터 초미세입자 (PM2.5) 및 미세입자 영역 (PM10)의 부유상입자물질을 황사기간 (3월)과 비황사기간 (4월)에 걸쳐 채집하였다. (중략)

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Geomorphic Development of Mt. Yeontae at Gampo area, Gyeongju City in the southeastern Korea (경주시 감포지역 해안단구 지형발달)

  • 윤순옥;황상일
    • Proceedings of the KGS Conference
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    • 2004.05a
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    • pp.39-39
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    • 2004
  • 한반도 동해안 지역은 해안단구가 모식적으로 분포하여 이에 대한 연구가 활발하게 이루어 졌다. 1973년에 김서운에 의해 처음으로 한반도에 해안단구가 보고되었으나, 오랫동안 해안단구는 구정선고도 약 90m a.5.1.에서 형성된 것이 가장 높은 것으로 간주되었고 그 이상 고도에서는 확인되지 않았다. 이후 황상일 외(2000)는 경주 감포에서 110, 120, 130, 150m의 지형면이 존재할 가능성을 보고했으며, 강릉 정동진에서 윤순옥 외(2003)에 의해 고고위면이 110, 140m에서 확인되었다. (중략)

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Historical earthquake data of Korean (한반도의 역사지진자료)

  • Lee, Gi Hwa
    • Journal of the Korean Geophysical Society
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    • v.1 no.1
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    • pp.3-22
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    • 1998
  • Korea boasts of abundant historical earthquake records of almost 1900 events. The epicenters and intensities of these earthquakes are determined on the basis of descriptions and felt areas of the events. It turns out that most of the earthquakes occurred on major faults or tectonic boundaries of the peninsula except for the northeastern part which had been the least disrupted by tectonic disturbances during the Mesozoic. It appears that the crustal layers of the southern and northwestern parts of the peninsula had been severely ruptured during the Mesozoic disturbances and some of the faults thus generated have been active since. The seismicity of the peninsula had been rather low from the first to the fourteenth century, but unusually high from the fifteenth to the eighteenth century, and have been rather low since. This period of unusually high seismicity of the peninsula coincides with that of the northeastern part of China, suggesting the two areas are seismologically closely connected. It appears that most of the seismicity of the peninsula results from the high stress propagating from the Himalayas where the Eurasian and Indian plates collide. The data file of Korean historical earthquakes is not yet complete and supplementary studies are under way. The main purpose of this paper is to provide the data file of Korean historical earthquakes analyzed up to date for geoscientists and engineers in need of this file.

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한반도 공급망 이익경영 모델 구축방안

  • Kim, Tae-Ho
    • Proceedings of the Safety Management and Science Conference
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    • 2009.11a
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    • pp.145-159
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    • 2009
  • 남북한 경제통합 시에 이익지대 확대 방안을 모색하고, 남북한 경제의 발전적인 방안을 탐구하고자 한다. 한반도 공급망 이익지대를 분석하여 공급망 이익지대 확대 전략을 수립하고자 한다. 그리고 한반도의 경제통합 시에 경제적인 손실과 낭비, 시행착오를 줄이고 경제발전의 부흥기를 도모하기 위함이다. 현재 북한지역의 무게 중심지를 분석하고 향후에 인구의 유동에 의해 초래될 무게중심지를 시나리오 기법으로 분석하여 위험요인을 최소화 하고자 한다.

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The Crustal and Upper Mantle Velocity Structure of the Southern Korean Peninsula from Receiver Functions and Surface-Wave Dispersion (수신함수와 표면파 분산의 동시역산을 이용한 한반도 남부지역의 지각과 상부맨틀 연구)

  • Yoo, H.J.;Lee, K.;Herrmann, R.B.
    • 한국지구물리탐사학회:학술대회논문집
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    • 2006.06a
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    • pp.61-70
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    • 2006
  • 3-D S-wave velocity model in the southern Korean Peninsula is investigated by using the joint inversion of receiver functions and surface-wave dispersion. A peninsula average Rayleigh-wave phase velocity in the 10-150 seconds range and tomographic estimates of the Rayleigh and Love wave group velocities in the 0.5-20 seconds period range determined using a $12.5{\times}12.5\;km$ grid for the southern part of the peninsula are used for the inversion. Receiver functions were determined from broadband (STS-2), short-period (SS-1) and acceleration (Episensor) channels of 95 stations. The dense distribution of the stations in the Peninsula permits us to examine the 3-D crustal structure in detail. The inversion result shows the variation and characteristics of S-wave velocity in the crust and upper mantle of the southern Korean Peninsula very well.

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