• The Science & Technology
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• v.33 no.3 s.370
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• pp.21-21
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• 2000

바위는 겉과 속의 색깔이 다르다. 바위의 겉은 광물의 풍화로 색깔이 변하므로 그 속색깔을 알아보려면 망치로 풍화된 겉을 떼어내야 한다. 그래서 지질학자들은 이를 '백견이 불여일타'라고 한다. 그런데 요즘 지질학계에는 야외 지질조사를 기피하고 실내에서 시료를 분석하는 경향이 만연되고 있어 안타깝다. 지질학의 진리를 캐러 야외로 나가자.

• Proceedings of the KSEEG Conference
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• 2007.04a
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• pp.667-669
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• 2007

• Proceedings of the KSEG Conference
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• 2001.03a
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• pp.127-140
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• 2001

최근 지질공학의 다양한 분야에 영상처리기법들이 적용되고 있다. 그러나 영상의 획득 및 분석 단계에서 발생하는 각종 오차에 관한 문제는 많은 부분 무시되어 왔다. 이에 본 연구에서는 암석영상처리의 신뢰도 향상을 위한 컬러보정기법을 개발하였다. 표준 컬러차트를 이용하여 컬러보정과 오차분석을 수행하였으며, 그 결과 영상처리의 신뢰도 향상과 영상들간의 상호 비교·분석을 꾀할 수 있었다.

• Journal of the Korean earth science society
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• v.38 no.6
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• pp.421-426
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• 2017

In this study, we selected three representative granite samples and conducted petrological observation to establish the Korean geostandards. Samples were taken from the two Jurassic (KJG-1, KJG-2) and one Cretaceous (KCG-1) granites in South Korea. The powder samples were prepared by the standard pulverization process, and glass beads were made for geochemical analysis using X-ray fluorescence (XRF) method, and finally, major element contents of the samples were acquired. The analytical data are shown with mean, standard deviation and relative standard deviation. The accuracy of the analysis was confirmed within an estimated error range of about 5% by comparing the recommended true values of the USGS and GSJ geostandards. Also, we checked the analytical precision by calculating a relative standard deviation of about 3% from the XRF analytical results for the three samples.

• Proceedings of the KSEEG Conference
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• 1999.04a
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• pp.184-186
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• 1999

• Proceedings of the KSEEG Conference
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• 2007.04a
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• pp.252-254
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• 2007

• Proceedings of the KSEEG Conference
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• 2007.04a
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• pp.549-551
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• 2007

• Proceedings of the KSEEG Conference
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• 2007.04a
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• pp.444-446
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• 2007

• Economic and Environmental Geology
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• v.48 no.4
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• pp.313-324
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• 2015

This study constructed a 3D geological model for Uggi Nuur Fe-Mn mineralization zone in Mongolia, and the 3D geological distribution is cross-analyzed with magnetic anomaly distribution to figure out relationship between ore zone and subsurface geology. As a result of 4 step 3D modeling procedures including geological cross section, surface modeling, foliation modeling and solid modeling, the geology of the both study area is bordered by faults in NW direction with Munguntessj formation being located in the west side of the fault while Yashill formation is located on the other side of the fault. Moreover, the strike direction of foliation in the both formation shows same directional pattern with the NW faults. The magnetic anomaly distribution reveals that higher anomaly values are concentrated to near the ground surface. The analyses of 3 dimensional distribution between subsurface geology and magnetic anomaly indicates that higher anomaly is mainly distributed over the Munguntessj formation as a elongated lens bodies whereas the magnetic anomaly is evenly found in the both of Munguntessj formation and Yashill formation in the study area 2. It infers that volcanic activities associated mineralization occurred during silurian period, and the mineralized zone is thought to be realigned along the geological structures caused by later stage tectonic activities.

• Journal of The Korean Association For Science Education
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• v.37 no.3
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• pp.465-481
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• 2017

This study is a research synthesis analyzing how field geology education is conducted in domestic and foreign countries in the recent 20 years and how it reflects the characteristics of authentic geologic inquiry. For these purposes, we first drew five elements of inquiry in field geology (observation, representation, abductive reasoning, spatial thinking, and diachronic thinking) considering the field geologists' actual research method as well as its pedagogical significance in science education. We developed analysis criteria for field geology education. The 53 cases were analyzed based on each element of inquiry in field geology and its sub-elements, and also the tendency of overall elements. As a result, observation and representation were included in most cases, but there appeared less frequency in order of abductive reasoning, spatial thinking, and diachronic thinking. For observation, the ratio of purposive observation and autonomous observation is high. For representation, both visualizing and linguistic type of representation and free-form representation appear frequently. For abductive reasoning, the step of generating hypothesis is often included and the hypothesis tends to be about the geological formatting process. For spatial thinking, type of self-location and perception of the spatial configuration of the structure appear at a high rate. For diachronic thinking, type of stratigraphic sequence is the most frequent. The proportions of the cases including three or more elements of inquiry in field geology consist 87% of the total. We suggested implications for improving geological fieldwork as authentic science inquiry in the future.