• 콘크리트학회논문집
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• 제21권2호
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• pp.121-127
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• 2009

연화재료의 변형률 국부화 거동에 따른 파괴영역과 파괴영역 내에서의 변형률 추이는 구조물의 극한거동에 큰 영향을 미치지만 파괴영역의 예측과 영역 내에서의 변형률을 정량화하는 것은 실험적으로 명확히 구명되어 있다고 보기 어렵다. 이 연구에서는 국부화된 파괴영역 및 그 영역 내에서의 변형률 분포 추이를 추정하기 위해 화상처리기법을 이용하였다. 화상처리기법의 신뢰성 및 타당성을 검증하기 위해, 일축압축공시체를 대상으로 화상처리기법을 이용하여 변형률을 추정하고, 이를 콘크리트 게이지로부터 취득한 변형률과 비교분석하였다. 분석 결과를 바탕으로 전단압축파괴형 보의 정적파괴실험에 화상처리기법을 적용하여 실험체의 거동에 따른 주인장변형률 및 주압축변형률의 분포도를 작성하였다. 마지막으로 작성된 분포도를 이용하여 국부화영역 및 국부변형률을 추정하였다. 실험 결과, 화상처리기법을 이용하여 취득한 파괴영역 내에서의 변형률 분포 추이는 비교적 정확히 실험체의 거동을 예측할 수 있었으며 손상 정도에 따라 비교적 합리적인 국부변형률값을 얻을 수 있었다.

• 자원환경지질
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• 제8권1호
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• pp.25-56
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• 1975

Most fluorite deposits of South Korea are distributed in three metallogenic zones namly as: Hwacheon, Hwangangni and Geumsan metallogenic zones. Fluorite deposits of each zone show The characteristic features owing to the geological setting, the structural patterns and their forming processes. deposits of the Hwacheon metallogenic zone are wholly fissure filling hydrothermal veins emThe bedded in shear fractures of the granite gneiss or schists of Precambrian age or in the cooling fractures of the granite and acidic hypabyssal rocks which are assumed to be a differentiated sister rock of the granite. Localization of most fluorite veins of the region is structurally controlled by NW and EW fracture systems and genetically related to the granite intrusion which ascertained as motivating rock of the fluorite mineralization. Fluorites are in most cases accompanied by quartz, chalcedony mainly and rarely agate, calcite, barite and sulphide base metals in some localities. The deposits of the Hwangangni metallogenic zone were formed at the last stage of hydrothermal polymineralization of W, Mo, Cu, Pb, Zn. The majority of the fluorite ore bodies were originated from replacement in limestone beds of Great Limestone Series or in calcareous interbeds of metasediments, whereas some cavity-filling ore bodies were embedded in phyllites and schists of the Ockcheon system and along the fissures in the replaced beds which were originated by volume decrease. The localization of fluorite deposits in this region is genetically related to the Moongyong granite which has been dated as middle Cretaceous, and controlled structurally by the $N20^{\circ}{\sim}50^{\circ}W$ extension fracture system or axial planes of folds, and by faults of NE direction that acted as paths of ore solution. The deposits of the Geumsan metallogenic zone are seemed to be formed through the similar process as that of Hwangangni metallogenic zone, but characteristic distinctions are in that they are more prevailing fracture filling veins and large number of the deposits are localized in roof-pendants or xenolithes of limestone in granites and porphyries. Igneous rocks that presumably motivated the mineraltzation are middle Cretaceous Geumsan granite and porphyries. Metallogenic epoch of the fluorite mineralization of South Korea are puesumably limited in early-middle Cretaceous. Studies of the fluid inclusions in fluorites of the region reveal that the homogenization temperature of the fluorite deposits are as follows: Hwacheon metallogenic zone : $95^{\circ}C{\sim}165^{\circ}C$; Hwangangni metallogenic zone : $97^{\circ}C{\sim}235^{\circ}C$; Geumsan metallogenic zone : $93^{\circ}C{\sim}236^{\circ}C$. Judging from the above results, the deposits of the Hwancheon region were formed at the epithermal stage, and those in the Hwangangni and Geumsan regions, were deposited at epithermal stage preceded by mesothermal mineralization of small scale in which some sulphide minerals were deposited. The analytical data of minor elements in the fluorites reveal that ore solutions of Hwangangni metallogenic zone seemed to be emanated in more acidic stage of magma differentiation than Hwacheon metallogenic zone did.