• 한국석유지질학회지
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• 제5권1_2호
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• pp.16-26
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• 1997

강원도 예미부근에는 예미각력암 (Yemi Breccia)이라는 층이 보고되어 있다. 이 층은 두위봉형 조선누층군 막골층을 부정합으로 덮고 있으며, 이 층 위에 고성 셰일이 정합적으로 놓인다고 알려져 왔다. 예미각력암의 야외조사와 조직적 관찰결과, 예미각력암은 막골층 상부가 퇴적될 당시에 퇴적된 증발암이 속성작용에 의해 용해됨으로써 생성된 속성산물인 용해-붕락 각력암 (solution-collapse breccia)이라 생각된다. 따라서 예미각력암은 기존에 독림된 층으로 제안된 바와는 달리 막골층의 상부층의 일부로 간주되어야 하며, 상위의 고성셰일은 직운산층으로, 고성석회암은 두위봉층과 대비되는 것으로 생각된다.

• 자원환경지질
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• 제2권3호
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• pp.58-67
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• 1969

Songgwang lead zinc mine is located in about 12km to the north-east of Jeonju City. Geology of the mine and its visinity is consisted of Jeonju series belonged to so-called Okcheon system, Seodaesan tuff formation, Silla series, and the quartz porphyry intruded into these formations. Jeonju series comprising 3 formations; that is, of Sadaeri, Sindong, and Girinbong. Jeonju series is generally distributed in southern part of the area, striking NNW, and diping NE $30^{\circ}$, or NW $30^{\circ}$. It is deformed to form synclinorium and anticlinorium plunging to the north with low angle. In the northern part of the area, Jeonju series was cut by Sinpeongri-fault of NEE direction near Sinpeongri. In the north side of the fault, it is overturned and shows NEE or NWW strikes and NW $60^{\circ}$ dips. At the west of Songgwangri, it is cut by 3 thrusts; the two are almost parallel each other, and the third oneis manifested by the fact that the lower black shale zone thrusted over the upper limestone. Songgwangri thrust, so named, is a post-mineral fault and its plane represents a premineral slip plane. Enrichment of are took place along the bedding plane or fissure parallel to it, as seen in adit No. 1 or No. 2 along the floor of the thrust, and along the sheared zone or the brecciated zone oblique to the plane near the thrust in crystalline limestone of Sindong formation as observed in the underground levels of inclined slope. Ore minerals are chiefly zincblende, galena, pyrrhotite, arsenopyrite, acompanied pyrite and chalcopyrite, and contain Au and Ag. In earlier stage of mineralization, the limestone was recrystalized, and sulphide minerals were enriched in the· permiable zone said above by pyrometasomatism, and in later stage the limestone was affected chloritization and sericitization. However hydrothermal replacement was weak, so that enrichment did not took place. It seems that minerallizing materials came up through the premineral slip plane and injected, and replaced the limestone in permiable zone said above with sulphide are minerals. Then Songgwangri thrust took place and, the lower black shale zone thrusted upon crystalline limestone.

• 한국세라믹학회지
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• 제48권6호
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• pp.584-588
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• 2011

In this work, effects of limestone powder on hydration of $C_3A-CaSO_4{\cdot}2H_2O$ system was discussed based on the XRD Quantitative analysis, and the possibility of Delayed Ettringite Formation was also discussed. The early hydration of $C_3A$ was delayed by addition of $CaCO_3$ powder. The delay effect was enhanced by increasing of $CaCO_3$ content and finer powder of $CaCO_3$ addition. After consumption of $CaSO_4{\cdot}2H_2O$, the reaction of $CaCO_3$ is started. Delayed Ettringite Formation would take place because monosulfoaluminate is not stable in presence of $CaCO_3$. In order to prevent the delayed ettringite formation in $C_3A-CaSO_4{\cdot}2H_2O-CaCO_3$ system, the reduction of monosulfoaluminate formation is important. Therefore, by increasing the amount of $CaCO_3$ addition and finer $CaCO_3$ powder addition, the delayed ettringite formation can be prevented.

• 자원환경지질
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• 제52권1호
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• pp.107-118
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• 2019

태백산분지 북익부 고품위 석회석의 생성은 크게 동생적(syngenetic)과 후생적(epigenetic) 관점으로 나뉘어 있으며, 산소-탄소 안정동위원소 비 특성을 이용하여 이들의 생성환경을 고찰하였다. 북익부의 4개 광산(GMI, 정선, 백운, 백광)과 남익부의 상동(오미아)광산, 그리고, 삼척지역의 쌍용동해광산을 대상으로 하였으며, 이들과의 비교를 위해 정선지역 대기층 노두시료를 포함하였으며, 이들을 색상에 따라 암회색, 회색, 담회색, 백색으로 구분하였다. 산소 안정동위원소 비는 4.5 ~ 21.6 ‰의 넓은 범위의 변화를 보이지만, 탄소 안정동위원소 비는 -1.1 ~ 0.8 ‰ (방해석 맥 제외)로 매우 좁은 범위를 보여, 열수의 작용이 크지 않았음을 지시한다. 또한, 광산별, 색상별 산소-탄소 안정동위원소 비의 분포범위의 차이는 없으며, 주변 노두에서 채취된 탄산염암과 유사한 범위를 보이는 것으로 보인다. 이와 같은 결과는 고품위 석회석의 생성에 있어서 열수의 영향은 거의 없었다는 것을 지시한다. 산소 안정동위원소 비 값은 암석의 색상변화(백색화)보다는 조직의 변화와 관련되는데, 산소 안정동위원소 비 15 ‰ 전후를 기준으로 탄산염암의 산상을 구분할 수 있다. 이보다 높은 경우 괴상 또는 층리가 잘 보존된 특징을 보이는 반면, 낮은 경우 하나의 시료 내에서 두 가지 이상의 색상이 나타나고 있으며, 층리는 교란되거나 거의 소멸하여 흔적만 확인된다. 두 가지 이상의 색상이 나타나는 경우 밝은 부분이 어두운 부분에 비해 현저히 낮은 산소 안정동위원소 비를 보이는 경우가 다수 관찰되며, 이는 열수와의 반응에 의한 현상으로 해석된다. 다만, 이와 같은 현상은 소규모로 나타나고 있으며, 광상 전체적인 고품위 석회석의 생성에 대한 해석으로는 적당하지 않다. 특히, 재결정화한 백색의 탄산염암에서 높은 산소 안정동위원소 비 값을 보이는 것은 이 지역 탄산염암의 재결정화에 열수의 작용이 매우 적었음을 지시하며, 주변 마그마에 의한 열적 영향만을 받은 결과로 해석된다. 또한, 고품위 석회석광상 내 광체의 분포가 수평으로 연속적이며, 고품위 석회석 상하 주변에 백운석이 층상으로 협재되는 등의 산상을 고려할 때, 연구지역 고품위 석회석의 생성은 동생적(syngenetic) 해석이 보다 더 타당할 것으로 판단된다. 따라서, 태백산분지 전반적으로 순차층서적 관점에 의한 퇴적상의 해석이 필요할 것으로 사료되며, 이는 추가적인 고품위 석회석 광체의 확보에 매우 중요한 요소가 될 것이다.

• 산업기술연구
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• 제21권A호
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• pp.251-256
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• 2001

This research is focused on an improvement of additional value of high grade limestone. To obtain the basic data of precipitated calcium carbonate(PCC), studies of physical properties of limestone, calcination and hydration characteristics, the characteristics to manufacture quick lime, hydrated lime, ground calcium carbonate and precipitated calcium carbonate were performed. In the carbonation process, formation of rombohedral must be kept under $10^{\circ}C$ for reaction. Although the temperature of reaction of lime milk was limited under $30^{\circ}C$ for a colloidal PCC manufacture, over $50^{\circ}C$ for spindle type PCC. The recommended reaction conditions for colloidal PCC are $20^{\circ}C$ of reaction temperature, 4% of $Ca(OH)_2$ concentration, 1000rpm of stirring rate and 200ml/min of $CO_2$ gas flow rate.

• 자원환경지질
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• 제16권1호
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• pp.37-49
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• 1983

The skarn type tungsten deposits are developed in the contact aureole of Jurassic biotite-hornblende granodiorite and limestone beds. The latter can be divided into the Great Limestone Series of Joseon System and Gabsan Formation which is correlative to the Hongjeom Series of Pyeongahn System. The skarns are impregnated in the limestone, sandstone, schist and granodiorite, and showing zonal distribution. The five skarn zones are from fresh limestone inwards to wollastonite-skarn, clinopyroxene-skarn, clinopyroxene-garnet skarn, garnet skarn and vesuvianite skarn zone. The ore mineral, scheelite, disseminates in the clinopyroxene-garnet and vesuvianite skarn zone, and the size of the scheelite crystals in vesuvianite skarn zone is larger than in clinopyroxene- garnet skarn zone. According to the mineral paragenesis and the composition of skarn minerals, oxygen fugacity ($fo_2$) is low. Fluid inclusions in quartz comprise much $LCO_2$ and fluid inclusion studies revealed that the homogenization temperatures range $240-290^{\circ}C$.

• 자원환경지질
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• 제6권4호
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• pp.219-230
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• 1973

This paper reviews Professor O.J. Kim's work on "The stratigraphy and geologic structure of the Great Limestone Series in South Korea". Although he stated in his paper such as "very few geologists in Korea argue without confident evidences against the age and stratigraphy of the Great Limestone Series which have been rather well established previously in most parts of the regions", he disregarded the Jeongseon type of the Joseon (Chosen) System and modified the Yeongweol and the Pyeongchang types. According to his description, the Jeongseon type is not a different type and it is only due to structural repetition of the Hwajeol and Dumudong Formations of the Duwibong type and its Maggol Limestone. Also, he devided the Sambangsan Formation of the Yeongweol type into the east and west parts along the so-called Jeolgaesan fault, and they are correlated to the Hongjeom Series and Sesong Slate (Seison Slate) of Kobayashi, respectively. Furthermore he established newly Yeongweol type which includes the original Kobayashi's Yeongweol type and the Upper Limestone of the Pyeongchang type. Also, he pointed out that his newly established Yeongweol type is quite correlatable to the Duwibong type. The writer's opinion can be concluded that the Jeongseon type is not simply of structural repetition and structurely the Sambangsan Formation can not be devided into two parts. Also structurely there is no evidence of its correlation to the Sesong Slate as well as his conodont study in his Yeongweol type shows no indication of the correlation. The writer thinks that as to the stratigraphy of the Yeongweol and Jeongseon types of the Joseon System, it should be agreed with the Kobayashi's opinion or should be followed the idea of the very few geologists, he mentioned.

• 한국건설순환자원학회논문집
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• 제11권4호
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• pp.364-372
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• 2023

본 연구에서는 시멘트 클링커의 소성 원료로서 조립의 석회석과 가공하지 않은 석탄재를 적용하여 시멘트 클링커의 미세구조 및 화학성분의 분포를 비교 고찰하였다. 시멘트 클링커의 원료로서 조립의 석회석을 적용한 시료는 시약급 원료를 사용한 시료에 비하여 소성성의 저하가 나타났으며, 석탄재를 적용한 시료에서는 소성성이 일부 증가하는 경향이 나타났다. 조립의 석회석과 석탄재를 적용한 시료에서 1350 ℃에서 Belite의 생성이 높게 나타났으며, 1350~1450 ℃의 구간에서 Belite에서 Alite로의 전환율이 높게 나타났다. 석탄재를 적용한 시료에서 1350~1450 ℃ 구간에서 간극상의 생성이 안정적으로 나타났다. 1350~1450 ℃로 소성된 시멘트 클링커의 미세구조 및 화학성분 분포는 모든 시료가 잘 발달 된 칼슘실리케이트상과 간극상이 명확하게 구분되는 형태 및 성분분포를 나타내었다.

• 동굴
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• 제62호
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• pp.35-41
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• 2004

• 한국콘크리트학회:학술대회논문집
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• 한국콘크리트학회 2005년도 봄학술 발표회 논문집(II)
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• pp.349-352
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• 2005

In this work, effects of limestone powder on hydration of $C_3A-CaSO_4\cdot2H_2O$ system was discussed based on the XRD Quantitative analysis, and the possibility of Delayed Ettringite Formation was also discussed. The early hydration of $C_{3}A$ was delayed by addition of $CaCO_{3}$ powder. The delay effect was enhanced by increasing of $CaCO_{3}$ content and finer powder of $CaCO_{3}$ addition. After consumption of $CaSO_4\cdot2H_2O$, the reaction of $CaCO_{3}$ is started. Delayed Ettringite Formation would take place because monosulfoaluminate is not stable in presence of $CaCO_{3}$. In order to prevent the delayed ettringite formation in $C_3A-CaSO_4\cdot2H_2O-CaCo_3$ system, the reduction of monosulfoaluminate formation is important. Therefore, by increasing the amount of $CaCO_{3}$ addition and finer $CaCO_{3}$ powder addition, the delayed ettringite formation can be prevented.