• 자원환경지질
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• 제19권3호
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• pp.179-192
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• 1986

In the Bupyeong district, Mesozoic pyroclastic rocks, intrusive breccia, granites and felsic porphyries comprise a volcano-plutonic complex, overlying and intruding the Precambrian Gyeonggi gneiss complex. pyroclastic rocks, consisted mainly of rhyolitic welded tuffs, form a topographic circular structure about 10 kilometers in diameter. Granites and felsic porphyries which intruded the pyroclastic rocks are distributed in the inner side and also along the outer margin of the circular structure. K-Ar ages of two granite bodies(biotite), 162 and $148{\pm}7$ Ma, and that of the intrusive rhyolite (whole rock), $121{\pm}6$ Ma indicate that a series of volcano-plutonic igneous activity occurred between Jurassic and early Cretaceous age. Petrochemical characteristics suggest that the pyroclastic rocks, granites and felsic porphyries were originated from the comagmatic source. From the evidences of field occurrence, petrochemical and geochronological characteristics of igneous rocks and the geologic structures, it is believed that the igneous rocks in the Bupyeong district were formed during a Jurassic to early Cretaceous resurgent caldera evolution.

• Molecules and Cells
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• 제20권2호
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• pp.167-172
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• 2005

Ceruloplasmin (Cp) is a copper protein with important functions in iron homeostasis and in inflammation. Cp mRNA expression is induced by interferon (IFN)-${\gamma}$ in U937 monocytic cells, but synthesis of Cp protein is halted after about 12 h by transcript-specific translational silencing. The silencing mechanism requires binding of a 4-component cytosolic inhibitor complex, IFN-gamma-activated inhibitor of translation (GAIT), to a defined structural element (GAIT element) in the Cp 3'-UTR. Translational silencing of Cp mRNA requires the essential proteins of mRNA circularization, suggesting that the translational inhibition requires end-to-end mRNA closure. These studies describe a new mechanism of translational control, and may shed light on the role that macrophage-derived Cp plays at the intersection of iron homeostasis and inflammation.

• 자원환경지질
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• 제14권3호
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• pp.123-142
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• 1981

Granitic complex in the Woosanbong area is composed of schistose granite, two-mica granite, biotite granite, porphyritic granite and pink feldspar granite in order of intrusion. In their boundary aspects, the gradational change between porphyritic granite and pink feldspar granite is observed in field relations. All the granites of the complex are classified to quartz monzonite by the modal compositions following Bateman's classification (1961) with the exception of pink feldspar granite which belongs to granite according to the petrographical classification. The first three granites are characterized by highly development of vein and/or lens-like pegmatites in their bodies, and two others contain green hornblende uniquely. These leucocratic two-mica granite shows an unusual character in ratio of muscovite to biotite 1: 0.7 to 1:13, and contains dominantly microcline. The content of muscovite varies in places in the field. Under the polarizing microscope it is revealed that the muscovite flakes occur as the products altered from biotite partly or completely, and it usually associates with chlorite flakes nearby. These features, therefore, suggests that biotite probably has been altered to muscovite and chlorite by hydration during deuteric processes. At the same stage, sericitization of plagioclase by the hydrolytic decomposition, and transformation of orthoclase to microcline may be taken place. Accordingly, it is obviously permissible to consider the two-mica granite as a kind of 'apo-granite' by deuteric alterations during the consolidation of magma.

• 자원환경지질
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• 제33권5호
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• pp.379-389
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• 2000

This study was focused on the investigation for the heavy metal contamination of soils derived from Yoecheon Industrial Complex in Chonnam Province. Total 201 soil samples including farmland, paddy, forest and playground soils were collected, extracted by 0.1N HCl and analyzed for Cd, Cu, Cr, Fe, Mn and Zn using AAS. Most pH values in soils were weak acidic ranges of 4-6, while some of them were over 8.0. Concentrations of Cd, Cu, Fe and Zn in the soils tend to be relatively high around the Au-Ag mine area, railroad stations and oil station, however, those of Cr, Mn and Pb show high at the northside of Pohang Steel Co (POSCO). Cadmium-Zn couples, and Cd-Zn and Zn-Cr couples have relatively good correlations in the farmland soils and paddy soils, respectively. Concentrations of Cd, Fe and Zn with depth tend to be higher in the top soils than in the bottom soils, but those of Cu and Pb do not show regular variations with depth.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 1998년도 공동 심포지엄 및 추계학술발표회
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• pp.119-122
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• 1998

Chemical analysis, measurement of pumping rates of 60 production wells and depth to water tables of 57 monitoring wells were carried to protect depletion of water resources and deterioration of water quality for the commercial portable ground-water. Borehole depth of production well averages 149m(31 boreholes), casing depth is 28m(29 boreholes), production rate is 70 $m^3$/day and depth to water table of monitoring well is 23.26m, respectively. The geology of 60 wells can be divided into Daebo granite(20), Okchun metarmorphic complex(18), Precambrian granitic gneiss(15), Bulguksa granite(4), Cheju volcanics(2), Cretaceous sedimentary rock(1). Average electrical conductivity and pH are 152$\mu$S/cm, and 7.35, respectively. The contents of major cation and anion predominantly $Ca^{2+}$>N $a^{+}$>M $g^{2+}$> $K^{+}$ and HC $O_{3}$$^{－}$ >S $O_{4}$$^{2-}$>Cl￣>F￣. Water type is predominantly $Ca^{2+}$-HC $O_{3}$$^{－}$(81.7%). It's possible that water chemistry of some wells were affected not only by the geology of boreholes penetrated but by inflows of surface water or shallow ground-water. Therefore, it is strongly necessary to steadily monitor the water quality and hydrogeologic conditins of production wells.ells.ls.ells.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 1998년도 Proceedings of International Symposium on Remote Sensing
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• pp.122-127
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• 1998

This paper presents the neuro-fuzzy classifier derived from the generic model of a 3-layer fuzzy perceptron and developed the classification software based on the neuro-fuzzl model. Also, a comparison of the neuro-fuzzy and maximum-likelihood classifiers is presented in this paper. The Airborne Multispectral Scanner(AMS) imagery of Tae-Duk Science Complex Town were used for this comparison. The neuro-fuzzy classifier was more considerably accurate in the mixed composition area like "bare soil" , "dried grass" and "coniferous tree", however, the "cement road" and "asphalt road" classified more correctly with the maximum-likelihood classifier than the neuro-fuzzy classifier. Thus, the neuro-fuzzy model can be used to classify the mixed composition area like the natural environment of korea peninsula. From this research we conclude that the neuro-fuzzy classifier was superior in suppression of mixed pixel classification errors, and more robust to training site heterogeneity and the use of class labels for land use that are mixtures of land cover signatures.

• 자원환경지질
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• 제51권5호
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• pp.409-428
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• 2018

영동지역은 지체구조상 옥천습곡대의 중앙 남동부와 영남육괴와의 경계부에 위치하며, 이들 경계부에는 백악기 영동 퇴적분지가 분포한다. 영동지역의 지질은 주로 선캠브리아시대 소백산 편마암복합체, 중생대 화강암류와 퇴적암류, 그리고 이들 암석을 부정합으로 덮은 제4기 충적층으로 이루어져 있다. 이외에도, 시대미상의 옥천누층군, 고생대의 퇴적암류, 트라이아스기의 화강암류들이 북서측에서 소규모로 산출된다. 이들 다양한 지질에서 산출되는 지하수 내 Rn 함량 특성을 검토하기 위해, 충적층/풍화대 지하수 관정 20개, 암반 지하수 관정 60개를 대상으로 2015년 8월 풍수기와 2016년 3월 갈수기 2 차례에 걸쳐 시료를 채취 분석하였다. 충적/풍화대 지하수의 Rn 함량은 백악기 반암 뿐 아니라 일부 쥬라기 화강암류와 소백산 편마암류 지역에서 높게 나타났다. 그러나, 상세 지질을 살펴보면, 쥬라기 화강암과 흑운모 편마암 자체보다는 인근의 백악기 반암과의 경계부 혹은 반암 인근의 관정 지하수에서 Rn 함량이 높게 나타나는 경향을 볼 수 있다. 암반 지하수에서의 상세 지질별로 Rn 함량 산출 특성을 살펴보면, 영동분지 내 백악기 퇴적암과 소백산 편마암복합체 중 흑운모 편마암과 편암 지역에서 Rn 함량이 적은 편이었고, 백악기 반암 자체, 트라이아스기 청산화강암과 복운모화강암의 경계부위, 쥬라기 화강암과 반암 경계부, 편마암 복합체 중 화강암질 편마암 혹은 화강편마암 지역에서 Rn 함량이 상대적으로 높게 검출되는 것들이 나타났다. 지하수 내 Rn 함량과 지질과의 연관성을 검토할 때, 개략적이고 큰 규모의 지질보다는 맥상 규모로 작은 규모와 이에 따른 정밀한 지질 상황을 고려할 때 지질 및 암종에 따른 Rn 함량의 변화 및 관련성을 의미있게 논의할 수 있을 것으로 판단된다. 또한, 지하수 관정이 위치한 지점에서의 지질 자체보다는 인근에 소규모로 산출되는 맥암, 페그마타이트, 석영맥 등의 산출 및 이들과 관련된 광화대/변질대 등 특수한 지질 상황을 고려한 지하수 수질 특성을 검토할 필요가 있다.

• 지질공학
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• 제15권3호
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• pp.281-288
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• 2005

본 연구에서 는 복소유전율상수 반응으로부터 벤토나이트 공시체의 물성치인 체적함수비와 수분분포 특성 을 파악하기 위하여 수행되었다. 벤토나이트 재료는 현재 폐기물처분장에서 차수재료로 널리 이용되고 있다. 차수재료의 경우, 일반적으로 투수계수가 $10^{-7}\;cm/sec$ 이하로 작아야 한다. 난투수성 재료에 대해 온도구배 에 따른 수분분포 특성을 파악하기 위해 FDR-V 측정 장비를 적용해 이들을 측정하였다. 그 결과, 복소유전율상수는 체적 함수비와 온도 증가에 따라 함께 증가함을 알 수 있었다. 온도구배 에 따른 복소유전율상수 변화는 수분이동이 온도가 높은 쪽에서 낮은 쪽으로 증가함을 확인하였으며, 이는 수분분포 특성을 보여 준 것이다.

• 자원환경지질
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• 제41권2호
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• pp.173-181
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• 2008

한반도 경기편마암 육괴내 서산층군과 시흥층군의 대표적인 변성암 시료에 대하여 CHIME 절대연령 측정을 실시하였다. 경기편마암복합체 변성암중의 모나자이트 CHIME연령은 234${\sim}$257 Ma로 페름기-트라이아스기 중기에 속하고 있다. 이 연령은 경기육괴내 흥성지역의 변성시기(231 Ma, Kim et al., 2006)와 오대산 지역의 변성시기(245${\sim}$248 Ma, Oh et al., 2006b)와도 조화적이며 남중국지괴와 북중국 지괴의 충돌에 의한 송림 변동으로 일어난 지각변동과 수반된 변성작용의 시대로 해석된다. 한반도의 경기육괴 서산층군과 시흥층군의 변성암의 변성연대는 다비-수루 충돌대의 변성 연대(220${\sim}$242 Ma, Yang et al., 2003; Liu et al., 2003, 2004) 보다 오래되며 이는 남중국과 북중국 지괴의 충돌이 중국대륙에서 보다 한반도 지역에서 선행되었을 가능성을 시사하고 있다.

• 자원환경지질
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• 제27권3호
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• pp.247-261
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• 1994

Honam Shear Zone is a mylonite zone approximately parallel to the NE-SW trend located southern part of Korea peninsula. Geologic ages and petrogenesis of foliated granites in this zone are as follows: Igneous rocks of this zone are composed of granite gneiss, Paleozoic granites, Songrim granites, Jurassic granites and Cretaceous granites. Foliated granites show deformed phase of Paleozoic and Songrim granites during Daebo Orogeny. And isotopic ages obtained from foliated granites are early Permian to late Triassic period (276~200 Ma). Most of foliated granite masses are igneous complex consisting of a series of differential product of cogenetic magma. The individual rock mass of foliated granites plotted on Harker diagram shows mostly similar trend of calc-alkali series. REE diagram indicates that LREE amount of foliated granites are more enriched than HREE and negative Eu anomalies of them are weaker than those of the other granites. From these data, we suggest the rocks are generated from continental margin under syntectonic environment. Original magma type of foliated granites correspond to I-type, syn-collision type and Hercyano type. In compressive stress field between Ogcheon folded belt and Youngnam massif, foliated granites had formed due to mylonitic deformation. Those facts indicate that magma of foliated granites would had been generated by melting in lower crust or contamination in upper mantle.