• Title/Summary/Keyword: IGSN71

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우리나라 육상 중역기점 전이

  • Choe, Gwang-Seon;Ok, Su-Seok;Won, Ji-Hun
    • Journal of the Korean Geophysical Society
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    • v.4 no.2
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    • pp.121-131
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    • 2001
  • We have established 88 auxiliary gravity reference stations by using two gravitimeters at the observation offices of the Korean meteorological agency and measured the locations by using GPS. All gravity values have been calculated on the basis of the gravity reference point at Pusan National University, thus, they have been established to bge easily converted to new absolute gravity value later. The increased numbers of the gravity reference stations will minimize errors due to measurements, drift correction etc. and increase the accuracy of the gravity data. The result of this research will be used to verify the gravity data which calculated with the relative gravity meter and to inspect relative gravity meters.

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A Study on the Crustal Structure of the Southern Korean Peninsula through Gravity Analysis (중력자료분석을 통한 한반도 지각구조에 관한 연구)

  • Kwon, Byung Doo;Yang, Su Yeong
    • 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.

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