• Economic and Environmental Geology
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• v.27 no.4
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• pp.397-409
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• 1994

The seemingly scattered plot of heat flow versus crustal thickness is explained by geodynamic processes and simple thermal relaxation in two contrasting tectonic elements. Elevated heat flow is characteristic of rift provinces where the crust is attenuated by stretching but also of orogenic belts where thrust tectonics thickens the crust and significantly enhances crustal heat production. With the progression of time, isostatic processes thin the thickened crust through uplift and erosion and thicken the rifted crust through subsidence and sedimentation. Heat flow relaxes to a value in equilibrium with background mantle heat flow.

• Proceedings of the KSEEG Conference
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• 2005.04a
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• pp.309-313
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• 2005

• Journal of the Korean Geophysical Society
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• v.5 no.4
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• pp.293-303
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• 2002

Applying elastic plate model, we estimated elastic thickness and rigidity of the lithosphere in southern part of the Korean Peninsula($332km{\times}332km$ area of which center is $36.5^{\circ}N$ in latitude and $127.5^{\circ}E$ in longitude) by analysing terrain data and gravity data measured up to 2002. We tried to exclude the East Sea in choosing the study area because it has different tectonic environment. The mean Moho depth was estimated to be 30 km by power spectrum analysis of gravity data in the study area, Assuming one layer crust and applying elastic plate model, the loads with wavelengths of greater than 300 km are locally compensated, loads with wavelengths in the range 80-300km are partially supported by the strength of the lithosphere, and loads with wavelengths of less than 80km are almost completely supported by lithospheric strength. Assuming crustal model and rigidity, we calculated predicted coherence and compared it with observed coherence. As a result, we wert able to estimate the effective elastic thickness to be of 15 km(corresponding flexural rigidity is $3.0{\times}10^{22}Nm$). This indicates that the crust of the study area is relatively weaker than other old and stable continental regions but is similar to continental margins or oceanic area. The low rigidity could be explained by many tectonic and thermal activities such as orogenic activities, magmatic intrusions, volcanic activities, foldings, faultings, etc.

• Journal of the Korean Home Economics Association
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• v.36 no.11
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• pp.193-207
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• 1998

이 연구의 목적은 아동의 연령과 성에 따른 아동의 역량지각 발달의 경향을 조사하고, 연령, 성을 포함한 가정환경과 또래 환경의 변수들의 역량지각에 미치는 영향을 구조평형 모델을 통해 알아 보았다. 또한, 이러한 역량지각의 발달 성향을 서구 문화권과 비교하여, 역량지각발달의 문화적 보편성이나 차이점을 알아 보고자 하였다. 유아, 또는 초등학교 저학년 아동은 면접으로, 그리고 3학년이상은 설문지를 사용하였다. 조사 대상은 유아, 초등학교 1, 3, 5학년, 중학교 1학년 아동 750명과 그들의 어머니이다. 인지, 사회, 신체 영역에서 모두 역량지각은 연령이 증가할수록 낮아졌다. 인지, 신체 영역의 역량지각에선 연령과 성의 상호작용효과가 나타났다. 그러나, 서구 문화권의 연구에서는 이러한 상호작용이 발견되지 않는다. 역량지각의 공변량구조모형에서는 또래환경 변수가 모두 포함시키기에 부적합한 변수로 나타났고, 연령, 성과 가족의 수입, 아버지의 교육수준, 가정의 물리적 환경, 부모의 정서적 지지가 아동의 역량지각에 의미 있게 영향을 미치는 것으로 나타났다.

• Proceedings of the KSRS Conference
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• 2000.04a
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• pp.55-60
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• 2000

인공위성의 Radar Altimeter 자료를 통해 국지적인 중력이상을 조사하기 위하여 ERS-1 Altimeter를 이용하였다. ERS-1 Radar Altimeter는 조밀하게 인접한 데이터 간격(~8km)을 갖고 있어서 전지구적 규모뿐만 아니라 국지적인 연구에도 적합하다. 연구대상지역은 세 개의 판이 만나서 지진과 화산활동이 활발하게 진행되는 필리핀판 지역(동경1$10^{\circ}$~150$^{\circ}$, 북위 0$^{\circ}$~30$^{\circ}$)을 선정하였다. 이 지역에 대한 해저의 지형과 중력 이상 분석을 통해 판구조 운동의 여러 증거를 파악할 수 있다. ERS-1 Radar Altimeter를 통해 얻어진 지오이드 높이(Geoid geight)는 후리-에어 중력이상(Free-air gravity anomaly)으로 쉽게 전환시킬 수 있다. 본 연구에서는 Fast Fourier Transform(FFT)을 이용하여 지오이드기복을 직접 후리-에어 중력이상으로 전환시키는 Direct conversion method를 사용하였다. 후리-에어 중력이상은 지각평형과 직접적으로 연관되어 지각보상의 정도를 파악할 수 있게 하며 일반적으로 해양의 분지는 지각평형상태로 있어서 평균적인 중력이상은 0mgal 근처로 나타난다. 그러나 본 연구에서 살펴본 국지적인 후리-에어 중력이상은 판구조론과 관련한 해구난 호상열도에서는 해양분지에서의 평균적인 값과 다른 중력이상의 양상을 나타내었다.

• 한국지구물리탐사학회:학술대회논문집
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• 2005.05a
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• pp.245-250
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• 2005

• Journal of the Korean earth science society
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• v.27 no.6
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• pp.620-642
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• 2006

The Moho structure and its deformation in the southern part of the Korean Peninsula were estimated using gravity and topography data. Gravity signals from the upper and lower crust were separated using a filter that was computed from isostacy and elastic thickness. The result of this study shows three characteristic features of the Moho deformation. First, the Moho folding structure is parallel to SKTL (the South Korean Tectonic Line), which indicates positive association with the collision of the Yeongnam and Gyeonggi Massifs and repeated compression afterwards. In contrast, noticeable deformation of the Moho was not observed along the Imjingang Belt, which is interpreted as another continental collisional belt in the Korean Peninsula. Second, the Moho beneath the Gyeongsang Basin has remarkably risen; this seems to be the result from both the collisional compression and buoyancy caused by magmatic underplating. Third, the Moho deformation is shallowest in the east of the Taebaek Mountains and deepens toward the west, consistent with the topographic characteristic of the Korean Peninsula of "high east and low west". It can be interpreted as the results of the opening of the East Sea and Ulleung Basin. A tectonic explanation for this could be the ascent of the mantle induced by continental rifting and horizontal extension at the early stage of the opening of the East Sea. The Moho deformation model computed in this study correlates well with the earthquake distribution and crustal movement measured by GPS. We suggest that the compression along the SKTL is still exerted, consequently, the Moho deformation is active, although it may be weak.

• Economic and Environmental Geology
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• v.18 no.4
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• pp.309-320
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• 1985

The crustal structure of the southern part of the Korean peninsula has been investigated based on the results of processing and anlaysis of gravity data. The processing techniques involve i) seperation of regional and residual anomalies by polynomial fittings, ii) power spectral analyses to determine the mean depth to the crustal base, iii) a filtering operation called "high-cut filtering and resampling," and iv) downward continuation to determine the undulation of the crustal base. The Bouguer anomalies show a lineation in the NE-SW direction which is the same as that of most mountains and tectonic lines of this area. The mean crustal depth is found to be 34km. The depth of the crustal base is varying in the estimated range of 26km to 36km with a thinner crust below the east coast than that of the west coast. The relief of the crustal base is appeared to be correlated with the regional surface topography. The linear regression relations computed between elevations and gravity anomalies indicate that the crust of this area seems to be not in perfect isostatic equilibrium but a little undercompensated state.

• Geophysics and Geophysical Exploration
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• v.22 no.1
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• pp.37-43
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• 2019

We present gravity anomaly maps based on KIGAM's gravity data measured from 2000 to 2018. Until 2016, we acquired gravity data on about 6,400 points for the purpose of regional mapping covering the whole country with data density of at least one point per $4km{\times}4km$ for reducing the time of the data acquisition. In addition, we have performed local gravity surveys for the purpose of mining development in and around the NMC Moland Mine at Jecheon in 2013 and in the Taebaeksan mineralized zone from 2015 to 2018 with data interval of several hundred meters to 2 km. Meanwhile, we carried out precise gravity explorations with data interval of about 250 m on and around epicenter areas of Gyeongju and Pohang earthquakes of relatively large magnitude which occurred in 2016 and in 2017, respectively. Thus we acquired in total about 9,600 points data as the result. We also used additional data acquired by Pusan National University for some local areas. Finally, gravity data more than 16,000 points except for the repetition and temporal control points were available to calculate free-air, Bouguer, and isostatic gravity anomalies. Therefore, the presented anomaly maps are most advanced in spatial distribution and the number of used data so far in Korea.

• Research in Vestibular Science
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• v.17 no.4
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• pp.134-141
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• 2018

Objectives: We aimed to study the role of vestibular input on spatial memory performance in mice that had undergone bilateral surgical labyrinthectomy, semicircular canal (SCC) occlusion and 4G hypergravity exposure. Methods: Twelve to 16 weeks old ICR mice (n=30) were used for the experiment. The experimental group divided into 3 groups. One group had undergone bilateral chemical labyrinthectomy, and the other group had performed SCC occlusion surgery, and the last group was exposed to 4G hypergravity for 2 weeks. The movement of mice was recorded using camera in Y maze which had 3 radial arms (35 cm long, 7 cm high, 10 cm wide). We counted the number of visiting arms and analyzed the information of arm selection using program we developed before and after procedure. Results: The bilateral labyrinthectomy group which semicircular canal and otolithic function was impaired showed low behavioral performance and spacial memory. The semicircular canal occlusion with $CO_2$ laser group which only semicircular canal function was impaired showed no difference in performance activity and spatial memory. However the hypergravity exposure group in which only otolithic function impaired showed spatial memory function was affected but the behavioral performance was spared. The impairment of spatial memory recovered after a few days after exposure in hypergravity group. Conclusions: This spatial memory function was affected by bilateral vestibular loss. Space-related information processing seems to be determined by otolithic organ information rather than semicircular canals. Due to otolithic function impairment, spatial learning was impaired after exposure to gravity changes in animals and this impaired performance was compensated after normal gravity exposure.