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      철광산의 광체 평가를 위한 지구통계학적 복합 모델링 = Geostatistical Approach to Integrated Modeling of Iron Mine for Evaluation of Ore Body

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      https://www.riss.kr/link?id=A100134079

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      다국어 초록 (Multilingual Abstract) kakao i 다국어 번역

      Evaluation of three-dimensional ore body modeling has been performed by applying the geostatistical integration technique to multiple geophysical (electrical resistivity, MT) and geological (borehole data, physical properties of core) information. It was available to analyze the resistivity range in borehole and other area through multiple geophysical data. A correlation between resistivity and density from physical properties test of core was also analyzed. In the case study results, the resistivity value of ore body is decreased contrast to increase of the density, which seems to be related to a reason that the ore body (magnetite) includes heavy conductive component (Fe) in itself. Based on the lab test of physical properties in iron mine region, various geophysical, geological and borehole data were used to provide ore body modeling, that is electrical resistivity, MT, physical properties data, borehole data and grade data obtained from borehole data. Of the various geostatistical techniques for the integrated data analysis, in this study, the SGS (sequential Gaussian simulation) method was applied to describe the varying non-homogeneity depending on region through the realization that maintains the mean and variance. With the geostatistical simulation results of geophysical, geological and grade data, the location of residual ore body and ore body which is previously reported was confirmed. In addition, another highly probable region of iron ore bodies was estimated deeper depth in study area through integrated modeling.
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      Evaluation of three-dimensional ore body modeling has been performed by applying the geostatistical integration technique to multiple geophysical (electrical resistivity, MT) and geological (borehole data, physical properties of core) information. It ...

      Evaluation of three-dimensional ore body modeling has been performed by applying the geostatistical integration technique to multiple geophysical (electrical resistivity, MT) and geological (borehole data, physical properties of core) information. It was available to analyze the resistivity range in borehole and other area through multiple geophysical data. A correlation between resistivity and density from physical properties test of core was also analyzed. In the case study results, the resistivity value of ore body is decreased contrast to increase of the density, which seems to be related to a reason that the ore body (magnetite) includes heavy conductive component (Fe) in itself. Based on the lab test of physical properties in iron mine region, various geophysical, geological and borehole data were used to provide ore body modeling, that is electrical resistivity, MT, physical properties data, borehole data and grade data obtained from borehole data. Of the various geostatistical techniques for the integrated data analysis, in this study, the SGS (sequential Gaussian simulation) method was applied to describe the varying non-homogeneity depending on region through the realization that maintains the mean and variance. With the geostatistical simulation results of geophysical, geological and grade data, the location of residual ore body and ore body which is previously reported was confirmed. In addition, another highly probable region of iron ore bodies was estimated deeper depth in study area through integrated modeling.

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      참고문헌 (Reference)

      1 박계순, "탄성파 자료의 해양분지 구조 해석 결과 향상을 위한 인공위성 중력자료의 지구통계학적 해석" 한국물리탐사학회 10 (10): 252-258, 2007

      2 박삼규, "지반의 전기비저항을 좌우하는 물성요인" 한국물리탐사학회 7 (7): 130-135, 2004

      3 오석훈, "암반등급 해석을 위한 비선형 지시자 변환과 3차원 크리깅 기술의 물리탐사 및 시추자료에 대한 적용" 한국지구과학회 26 (26): 429-435, 2005

      4 김성중, "베리오그램을 이용한 광체 평가 및 3차원 모델링 소프트웨어 개발" 한국자원공학회 46 (46): 151-159, 2009

      5 Katsube, T., "The electro-chemical transient phenomena of ore and rock samples (II) (An investigation of measuring apparatus and of transient phenomena of electrode)" 22 : 21-33, 1969

      6 Lee, S. M., "Petrogenesis and the syenite in the Yangyang mine district, Kangwon province" 4 : 199-214, 1968

      7 Lee, S. H., "Ore petrological studies on the genesis of the metamorphic iron deposits in southern Korea" 15 : 210-229, 1979

      8 Johnson, M., "Multivariate statistical simulation" Wiley 230-, 1987

      9 Goovaerts, P., "Geostatistics for natural resources evaluation" Oxford University Press 1997

      10 Choi, D. H., "Fe scrutiny report of Yangyang ironmine" KORES 2-5, 2010

      1 박계순, "탄성파 자료의 해양분지 구조 해석 결과 향상을 위한 인공위성 중력자료의 지구통계학적 해석" 한국물리탐사학회 10 (10): 252-258, 2007

      2 박삼규, "지반의 전기비저항을 좌우하는 물성요인" 한국물리탐사학회 7 (7): 130-135, 2004

      3 오석훈, "암반등급 해석을 위한 비선형 지시자 변환과 3차원 크리깅 기술의 물리탐사 및 시추자료에 대한 적용" 한국지구과학회 26 (26): 429-435, 2005

      4 김성중, "베리오그램을 이용한 광체 평가 및 3차원 모델링 소프트웨어 개발" 한국자원공학회 46 (46): 151-159, 2009

      5 Katsube, T., "The electro-chemical transient phenomena of ore and rock samples (II) (An investigation of measuring apparatus and of transient phenomena of electrode)" 22 : 21-33, 1969

      6 Lee, S. M., "Petrogenesis and the syenite in the Yangyang mine district, Kangwon province" 4 : 199-214, 1968

      7 Lee, S. H., "Ore petrological studies on the genesis of the metamorphic iron deposits in southern Korea" 15 : 210-229, 1979

      8 Johnson, M., "Multivariate statistical simulation" Wiley 230-, 1987

      9 Goovaerts, P., "Geostatistics for natural resources evaluation" Oxford University Press 1997

      10 Choi, D. H., "Fe scrutiny report of Yangyang ironmine" KORES 2-5, 2010

      11 Kim, Y. H., "Experimental verification of factors affecting core resistivity measurements" 2 (2): 225-233, 1999

      12 Issaks, E. H., "An introductions to applied geostatistics" Oxford University Press 1989

      13 Kim, J. D., "A study of validation analysis for reopening of Yangyang iron-mine" Kangwon National University 18-19, 2009

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      학술지 이력

      학술지 이력
      연월일 이력구분 이력상세 등재구분
      2026 평가예정 재인증평가 신청대상 (재인증)
      2020-01-01 평가 등재학술지 유지 (재인증) KCI등재
      2017-01-01 평가 등재학술지 유지 (계속평가) KCI등재
      2013-01-01 평가 등재 1차 FAIL (등재유지) KCI등재
      2010-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2008-12-23 학술지명변경 한글명 : 물리탐사 -> 지구물리와 물리탐사
      외국어명 : Geophysical Exploration -> Geophysics and Geophysical Exploration
      KCI등재
      2008-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2006-01-01 평가 등재학술지 선정 (등재후보2차) KCI등재
      2005-01-01 평가 등재후보 1차 PASS (등재후보1차) KCI등재후보
      2003-01-01 평가 등재후보학술지 선정 (신규평가) KCI등재후보
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      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.15 0.15 0.15
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.14 0.15 0.311 0.07
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