• 지질공학
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• 제29권4호
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• pp.451-460
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• 2019

본 논문에서는 고상식(Piloti) 기초가 사용되는 오일샌드 플랜트의 하부기초에 소형강관 말뚝이나 마이크로 파일 등을 마찰 말뚝개념으로 사용할 경우 발생할 수 있는 문제점을 극복하고자 복합거동 연결체를 제안하였다. 말뚝의 개별 침하나 융기(Heaving)를 1개의 군으로 연결하여 복합거동이 가능하도록 하였으며, 하중 지지특성을 분석하였다. 기존 무리말뚝과 말뚝전면(Piled raft) 기초의 장점을 오일샌드 플랜트에 적용 할 수 있도록 복합거동 연결체의 형상을 결정하였다. 또한, 축소모형을 제작하여 하중에 대한 거동을 계측하고, 이를 통해 장치의 안정성 및 취약부위를 검토하여 연결체의 형태를 평가하였다.

• 한국광물학회지
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• 제30권3호
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• pp.127-136
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• 2017

자외선 차단기능과 제균 기능을 갖는 합성 $TiO_2$-복합체에 대해 압력의 영향을 체크하기 위해 고압실험을 시행하였다. 복합체 분말시료는 아나타제와 루틸 및 염화은으로 구성되어 있으며, 입자크기는 34 nm 정도로 결정되었다. 아나타제와 루틸 모두 약 14~16 GPa 구간에서 $ZrO_2$ (배델레이트)-형태의 결정구조로 상변이하며, 본 실험의 최고압력인 22.7 GPa까지 상변이는 계속된다. 압력을 모두 제거하여 상압 상태가 되면, 루틸은 ${\alpha}-PbO_2$ 구조로 상변이하며 아나타제는 고압의 $ZrO_2$-결정구조가 유지되는 것으로 판단된다. 염화은의 회절피크는 낮은 압력에서 사라지는 것이 관찰되었다.

• 자원환경지질
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• 제34권5호
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• pp.437-446
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• 2001

부산 보배견운모 광상의 프로필리틱 열수변질대에서 형성된 녹염석은 다양한 누대구조를 수반하는데, 다중결정성장 누대구조, 진동누대구조, patchy누대구조 및 강도가 약한 불규칙한 누대구조가 특징적이다. 누대구조는 주로 열수용 액의 AI Fe의 활동도에 좌우되며, 전반적으로 결정의 중심부에서는 AI, 가장자리에서는 Fe의 함량이 높다. 녹염석 의 Ps는 18.5-34.3 mot.% 범위이다. 여러 결정이 중첩하여 형성된 누대구조에서는 잔류조직이 부분적으로 흡수용해 되었으며, 이후에 결정들이 새로 성장하였다. 다중결정성장 누대구조나 진동누대구조는 열수시스템의 유체의 화학조성, 산화환원전위, 온도 등과 같은 물리화학적 변수들이 급격하게 변동하였음 지시한다

• 자원환경지질
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• 제30권2호
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• pp.153-161
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• 1997

Diagrams of $^{87}Sr/^{86}Sr$ versus Ba/Nb and MgO/FeO are scattered, and $^{87}Sr/^{86}Sr$ variation with the increase of $SiO_2$ are scattered in Gwangju granitoid. Diagrams of $(^{87}Sr/^{86}Sr)$i versus $(^{143}Nd/^{144}Nd)$i and ${\varepsilon}Nd$ versus 1/Nd variation are also scattered in Gwangju granitoid. It shows that the source magma of Gwangju granitoid are derived from partial melting materials of heterogeneous upper crust. Very low ${\varepsilon}Nd$ values (-15.19~-19.49) and very high ${\varepsilon}Sr$ values (92.72~308.85) mean that the source magma of Gwangju granitoid is derived from sedimentary substance melting. According to $(^{87}Sr/^{86}Sr)$ 180Ma, and the plot of ${\varepsilon}Sr$ versus ${\varepsilon}Nd$, the Gwangju granitoid shows that the source magma is derived from upper crust materials. Nd model ages of Gwangju granitoid (1.82~2.42G.A.) are older than meta-sediments of Okcheon formation (1.15~1.60G.A.) and similar or close to Pre-Cambrian gneiss complex of Ryoungnam massif (2.17~2.47G.A.or 2.11~2.38G.A.).Therefore, the source magma of the Gwangju granitoid could be derived from the partial melting of Pre-Cambrian gneiss complex of Ryoungnam massif.

• 자원환경지질
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• 제34권6호
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• pp.601-615
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• 2001

본 연구지역인 충북 보은군 보은읍 일대는 옥천변성대에 속하며, 도로공사구간 중 1:0.:리 구배로 절취한 암반사 면내의 일부구간에서 평면파괴가 발생하였다. 이 구간은 파괴면과 동일한 방향성을 갖는 불연속면에 의해 추가붕괴가 예상되는 등 불안정한 상태이다. 따라서, 본 사면에 대해 SMR, 평사투영법, 한계평형법으로 안전성을 해석하였다. 그러나, 이러한 방법으로 해석할 수 없는 절취에 따른 암반사면의 응력재분배 및 비선형적인 변위거동에 대해서는 UDEC 을 이용하여 수치해석하고, 보강공법을 적용하여 안정성을 해석해 보았다.

• 지질공학
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• 제24권2호
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• pp.237-246
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• 2014

경기도 가축매몰지 주변 지하수의 계절별 변동 특성과 원인 분석을 위하여 가축매몰지 주변 60 m 이내에 위치한 관정(84개소)을 선별하여 오염물질들의 분포 및 특성과 그 원인에 대한 분석을 수행하였다. 오염원에 대한 지시인자(pH, DO, ORP, EC)의 경우, 대부분의 관정에서 계절에 상관없이 비교적 일정한 값을 유지하고 있는 것으로 나타나 침출수와 같은 오염원에 의한 계절적 영향이 뚜렷하지 않은 것으로 분석되었다. 질산성질소의 경우 대부분 30 mg/L 내외의 농도분포를 보이는 것으로 나타났으며 특히 가축매몰지로부터 20 m 이내에 위치한 관정에서도 15 mg/L 이하의 농도 분포를 보이는 것으로 분석되었다 암모니아성질소와 염소이온의 경우 가축매몰지와 근접한 곳에 위치한 관정보다는 오히려 40 ~ 60 m 거리에 위치하는 관정에서 더 높은 농도 분포를 보이는 것으로 나타났다. 이러한 결과는 대부분 가축매몰지 침출수와 같은 높은 농도의 오염물 유입보다는 각 관정 주변에 위치한 기존의 오염에 의한 영향을 나타내주는 것이라 할 수 있으며 향후 가축매몰지 관련 지하수 보전 및 관리에 있어서 유용한 정보를 제공해 줄 수 있을 것으로 기대된다.

• 자원환경지질
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• 제6권4호
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• pp.201-216
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• 1973

Being believed thus far to be distributed in the wide areas in the vicinity of Seoul, the capital city of Korea, the Yonchon System in its type locality in Yonchon-gun from which the name derived was never previously traced down or correlated to the Precambrian metamorphic complex in Seoul area where the present study was carried out. Due to in accessibility to Yonchon area, the writer also could not trace the system down to the area studied so as to correlate them. The present study endeavored to differentiate general stratigraphy and interprete the structure of the metamorphic complex in the area. In spite of the complexity of structure and rapid changes in lithofacies of the complex, it was succeeded to find out the key bed by which the stratigraphy and structure of the area could be straightened out. The keybeds were the Buchon limestone bed in the western parts of the area; Daisongri quartzite bed cropped out in the southeastern area; Jangrak quartzite bed scattered in the several localities in the northwest, southwest, and eastern parts of the area; and Earn quartzite bed isolated in the eastern part of the area. These keybeds together with the broad regional structure made it possible to differentiated the Precambrian rocks in ascending order into the Kyonggi metamorphic complex, Jangrak group and Chunsung group which are in clinounconformable relation, and the first complex were again separated in ascending order into Buchon, Sihung, and Yangpyong metermorphic groups. Althcugh it has being vaguely called as the Yonchon system thus far, the Kyonggi metamorphic complex have never been studied before. The complex might, however, belong to early to early-middle Precambrian age. The Jangrak and Chunsung group were correlated to the Sangwon system in North Korea by the writer (1972), but it became apparent that the rocks of the groups have different lithology and highly metamorphosd than those of the Sangwon system which has thick sequence of limestone and slightly metamorphosed. Being deposited in the margin of the basin, it is natural that the groups poccess terrestrial sediments rather than limestone, yet no explanation is at hand as to what was the cause of bringing such difference in grade of metamorphism. Thus the writer attempted to correlate the both groups to those of pre-Sangwon and post-Yonchon which might be middle to early-late Precambrian time. Judging from difference in grade of deformation and unconformity between the Kyonggi metamorphic complex, Jangrak group, and Chunsung group, three stages of orogeny were established: the Kyonggi, Jangrak orogenies, and Chunsung disturbance toward younger age. It is rather astonishing to point out that the structure of these Precambrian formations. was not effected by Daebo orogeny of Jurassic age. The post-tectonic block faulting was accompanied by these orogenies, and in consequence NNE and N-S trending faults were originated. These faulting were intermittented and repeated until Daebo orogeny at which granites intruded along these faults. The manifestation of alignment of these faults is indicated by the parallel and straight linear development of valleys and streams in the Kyonggi Massifland.

• 자원환경지질
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• 제10권3호
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• pp.107-117
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• 1977

The Charyong batholith extends northeasterly from the west coast to the west of Wonju in the central parts of Korean Penninsula. The batholith is separated by the metamorphic complex into the northern and the southern granites. and is believed to intrude during the Daebo orogeny of early Jurassic to early Cretaceous age. It constitutes a sort of anticlinorium and the metamorphic complex can be regarded as a huge roof pendant. The modal analysis indicates that the Charyong batholith belongs to a series of adamellite-granodiorte-to-nalite. The oxidation property happened during a magmatic segregation reveals that the batholith shows in general orogenic assimilation trend. The granites of early to middle Jurassic age show orogenic assimilation trend, whereas those of late Jurassic to early Cretaceous age post orogenic noassimilation trend. The fracture system of the whole region is two folds: the fractures having attitute of $N25{\sim}40^{\circ}E$ and $70^{\circ}SE$ are regarded as tension fractures, and those of NS, and 50E to vertical and $N50^{\circ}E$ and $80^{\circ}E$ to vertical as shear fractures. All these facts suggest definitely that the Charyong batholith is the syntectonic intrusives during the Daebo orogeny. The mineral deposits in the area studied are gold-silver deposits in majority which was named by O,J.Kim(1970) as the Chonan metallogenic province. They are sulfides baring quartz veins which were emplaced along the tension and shear fractures originated by the Daebo orogeny.

• 자원환경지질
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• 제27권2호
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• pp.131-145
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• 1994

The Daehung and Pyeongan talc mines are located in the Yoogoo area, Chungcheongnam-Do. These deposits occur as the complex vein type in the ultramafic rocks which intruded Precambrian gneiss. The talc ore formed from sepentinitt: originated from ultramafic rocks but some of those from hornblende gneiss. The talcification processes were considered here on the basis of the mineral assemblages, paragenesis, and geochemistry. It appears that there are five processes in talcification ; serpentine$\rightarrow$talc, phlogopite$\rightarrow$chlorite$\rightarrow$talc, phlogopite$\rightarrow$talc, hornblende$\rightarrow$chlorite$\rightarrow$talc, and hornblende$\rightarrow$talc. Among them, the most dominant alteration path is serpentine to talc in these deposits. EPMA data suggest that there might be interstratified minerals were in between parent mineral and talc such as serpentine and talc, and phlogopite and talc. It can be found that tremolite exists in between the inner and outer most part of talcified serpentinite blocks coated with phlogopite. Some of tremolites has been altered to talc. The quartz veins and carbonate minerals were found in the talc ore zone. It indicates that the hydrothermal solution played an important role in talcification. The hydrothermal alteration occured after sepentinization. Ore zones can be divided into two zones; talc-serpentine zone preserving a pseudormorph of olivine (mesh texture) and talc-phlogopite zone showing talcification from phlogopite directly or through chlorite. It can be concluded that the formation of major talc ore body was due to talcification of serpentinite and phlogopite by hydrothermal solution. A nature of hydrothermal solution was relatively pure water at the beginning of serpentinization, and was getting richer in silica composition. There was a large amount influx of K and AI with hydrothermal solution in the later stage, and increased $P_{CO_{2}}$ also. It suggests that phlogopite formed in later stages as a secondary mineral. So, the major part of the talc ore body was formed from one parents rocks, serpentinite originated from ultramafic rocks, by hydrothermal solutions at several times.

• 자원환경지질
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• 제28권6호
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• pp.541-551
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• 1995

The Yeongdeog gold-silver deposits at Jipum, Gyeongsangbugdo, is of a middle Paleogene $(45.52{\pm}1.02Ma)$ vein type, and is hosted in shale and sandstone of Cretaceous age. Based on mineral paragenesis, vein structure and mineral assemblages, the ore mineralization can be divided into two distinct depositional stages. The early stage is associated with base-metals such as pyrite, arsenopyrite (27.99~30.99 at%), hematite, rutile, pyrrhotite, sphalerite (10.53~18.42 FeS mole%), chalcopyrite and galena with wallrock alteration such as chlorite, sericite and pyrite. The late stage is characterized by the Au-Ag mineralization such as electrum, Ag-bearing tetrahedrite, freibergite, pyrargyrite, unidentified mineral, pyrite, sphalerite (1.08~5.57 FeS mole%), chalcopyrite and galena. Fluid inclusion data indicate that fluid temperatures and salinities range from 343 to $227^{\circ}C$ and from 8.3 to 5.7 wt% eq. NaCl in early stage, respectively. Temperatures and salinities of NaCl eq. wt% range from 299 to $225^{\circ}C$ and from 12.9 to 4.3 in late stage, respectively. They suggest that complex cooling histories were occured by the mixing of the fluids. Sulfur fugacity $(-logfs_2)$ deduced by mineral assemblages and composition ranges from 8.3 to 14.7 atm. in early stage, and from 8.8 to 14.5 atm. in late stage. It suggests that the mineralization was related to decrease of temperature in early stage and fluctuations of $fS_2$ with decrease of temperature in late stage. Sulfur and oxygen isotope compositions are 4.48~5.60‰ and 9.25~10.8% in early stage, and late stage is 4.84~7.00‰ and 5.7‰, respectively. It indicated that hydrothermal fluids may be magmatic origin with some degree of mixing of another water during paragenetic time.