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

• Proceedings of the KSEEG Conference
• /
• 2007.04a
• /
• pp.541-542
• /
• 2007

• Journal of the Speleological Society of Korea
• /
• v.1 no.1
• /
• pp.23-26
• /
• 1975

본논문은 한반도내에 분포하는 수종의 동굴의 분포형태와 그의 성인 및 발달과정을 성인론적으로 해석하고 그들에 대한 연구를 하는데 있어서 지질학적인 문제점을 제시하는데 있다. (중략)

• Proceedings of the KSEEG Conference
• /
• 2000.04b
• /
• pp.233-234
• /
• 2000

• Economic and Environmental Geology
• /
• v.37 no.4
• /
• pp.391-400
• /
• 2004

The purpose of this study is to analyze the geothermal anomaly based on the relationship between heat flow values and geologic settings in South Korea. For this, a total of 247 heat flow data was constructed to spatial database and the spatial database was overlaid with 1 : 1,000,000-scale digital geologic map using GIS. As the result, the average of heat flow is 64$\pm$14mW$m^{-2}$in South Korea. In the lithological aspect, the area of sedimentary rock shows high heat flow of 74mW$m^{-2}$, sedimentary/volcanic rock area 62mW$m^{-2}$, plutonic rock area 63mW$m^{-2}$ and metamorphic rock area 61mW$m^{-2}$. In the geologic time sequence, the Cenozoic strata has 91mW$m^{-2}$, the Mesozoic and Paleozoic strata 65mW$m^{-2}$, the Proterozoic strata 55mW$m^{-2}$ and the Archean strata 61mW$m^{-2}$.

• The Journal of Engineering Geology
• /
• v.33 no.3
• /
• pp.475-487
• /
• 2023

We surveyed the distribution of soil layers on Dongdo and Seodo of Dokdo and measured the physical properties of the soils. To investigate the distribution of soil layers, the soil depth was measured directly in accessible locations, and visual observations of inaccessible locations were carried out using drones and boats. Soil depths ranged from 3 to 50 cm, and most soil layers had depths of 10~20 cm. Based on these results, a map of the soil layer was drawn using 5 cm intervals for soil depth. To analyze the soil characteristics of Dokdo, soil samples were collected from 13 locations on Dongdo and 13 locations on Seodo, in consideration of various geological settings. According to the results of grain size distribution tests, sand contents were >75%, and soil from Seodo contained more gravel-sized particles than that from Dongdo. Using the unified soil classification system (USCS) and textural classification chart of the United States Department of Agriculture (USDA), most of the soil samples from Dokdo are classified as sand, and some are classified as loamy or clayey sand. In addition, well-graded loamy or clayey sands are more common in Dongdo, and poorly graded sands with gravel are more common in Seodo. These results are expected to be important for studying soil characteristics on Dokdo.

• Journal of Plant Biology
• /
• v.35 no.3
• /
• pp.219-227
• /
• 1992

Formation, cellular distribution and structural changes of storage lipid, and active site and cellular localization of lipase in endosperms and cotyledons of lipid-rich seeds such as Helianthus annuus, Ricinus communis and Pinus koraiensis, and in those of starch-rich seeds such as Pisum sativum and Zea mays were investigated in relation to the seed development by cytochemical methods. In endosperms and storage cotyledons of lipid- and starch-rich seeds after seed-gathering, there were widely distributed storage material which was composed of spherical protein bodies, spherosomes, and starch granules. But cellular organelles were hardly observed in the cytoplasm. Staining pattern of vesicles released from SER, and of low electron dense membraneous granules, which were perhaps at an early stage of spherosomes, were the same as in the spherosome. Electrondense granules released from RER were observed in the vicinity of plasma membrane. As a result of lipid staining, the spherosomes were more electron dense and were uniform as compared with the protein matrix within the protein body and cytoplasmic proteinaceous granules. The major component of the spherosome was determinated to be lipid. Spherosomes and vesicles containing SER-released materials showed the same as in the electron density. Lipase activity was especially strong in the inner region and on the surface of decomposed spherosomes and near the plasma membrane.mbrane.

• 한국석유지질학회:학술대회논문집
• /
• autumn
• /
• pp.31-31
• /
• 2000

• Proceedings of the KSEEG Conference
• /
• 2001.04a
• /
• pp.332-335
• /
• 2001

• Proceedings of the Korean Radioactive Waste Society Conference
• /
• 2004.06a
• /
• pp.226-227
• /
• 2004

본 연구에서는 원자력 연구소 내에 건설할 고준위 폐기물 지하처분연구시설 부지에 관한 특성을 파악하고, 연구시설의 위치를 선정하기 위한 지질학적 연구를 실시하였다. 지표지질조사를 통하여 연구소 내에 분포하는 암석들의 분류와 선구조 분석을 실시하였고, 지구물리탐사와 시추조사를 통한 지하 암반의 분포양상과 연구시설 주변의 추정되는 파쇄대의 분포를 확인하였다. 지표지질조사결과 복운모화강암과 화강섬록암질 편마암이 점이적인 관계로 분포하고 있으며 (Fig.1, 3), 이들 화강암류 내에는 암맥상으로 중성 혹은 염기성 암맥들이 절리의 방향과 동일하게 관입 분포한다. 절리의 방향성은 N30E, N80W, NS방향으로 분포하고 있다(Fig. 2).(중략)