• 광물과 암석
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• 제34권2호
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• pp.147-156
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• 2021

몽골 남부 구르반사이한 호상 열도 지형 내 족도르 지역의 함동 석영맥에 대한 유체포유물 연구 결과를 보고한다. 족도르 지역에는 후기 백악기 퇴적층 내에 정치된 화강섬록 반암 내에 구조적으로 제어되는 동 광화작용이 나타난다. 이러한 화강섬록 반암 내에 동 광물 함유 석영맥은 프로필리틱 변질대의 석영-녹렴석-자철석 및 석영-자철석을 포함하는 열수 변질 양상을 보인다. 석영맥은 광물 조합에 따라 두 가지 유형으로 분류되며 주로 황동석과 함께 산출되고 드물게는 반동석, 자철석, 황철석과 함께 산출된다. 석영-자철석±황동석 및 석영-녹렴석-자철석 조합의 석영맥 내 유체포유물은 기포 크기 5-30 vol.%, 염농도 2-13 wt.% NaCl, 균질화 온도 107-270℃인 2상의 수성 포유물이다. 관찰된 석영맥의 광물 조합과 모암의 지구화학적 특성 및 변질 양상 등으로 판단했을 때, 유체포유물 자료는 연구 지역이 반암동 관련 광화작용의 프로필리틱 변질 영역에 해당함을 보여준다.

• 현장농수산연구지
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• 제21권1호
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• pp.15-28
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• 2019

담수재배 시 배양토로 하이드로 볼과 맥반석의 부피 비율이 도자기 분 식물의 생장에 미치는 영향을 알아보기 위하여 해송(Pinus thunbergii Parl), 진백(Juniperus chinensis L. var. sargentii Henry), 목서(Osmanthus fragrans Lour.), 장수매(Chaenomeles japonica Lindl. ex Spach) 등 4종에 대하여 실험을 하였다. 배양토 비율에 따른 해송, 진백, 목서, 장수매의 생존율은 해송과 장수매는 하이드로볼 80% + 맥반석 20%에서 100%였으며 진백과 목서는 하이드로볼 20% + 맥반석 80%에서 100%와 80.0%로 높은 생존율은 보였으나 대조구인 물 및 마사토의 생존율은 해송, 진백, 장수매에서 80%이하의 생존율을 보였으며 특히 목서의 경우 50%이하의 낮은 생존율을 보였다. 배양토 비율에 따른 생체중 증가율은 해송과 장수매가 하이드로볼 80% + 맥반석 20%에서 각각 58.6%와 15.8%로 가장 높았으며 하이드로볼의 함량이 증가할수록 생체중 증가율이 높은 것으로 나타났다. 진백과 목서의 경우 하이드로볼 20% + 맥반석 80%에서 생체중 증가율이 각각 71.4%와 59.7%로 높게 나타났으며 맥반석의 함량이 증가할수록 생체중 증가율이 높아지는 것으로 나타났다. 대조구인 마사토의 생체중 증가율은 해송, 진백, 목서, 장수매에서 각각 32.7%, 48.0%, 33.3%와 7.0%로 가장 낮은 생체중 증가율을 보였다. 이와 같이 담수재배 배양토로 대조구인 마사토는 낮은 생존율과 생체중 증가율을 보였다. 하지만 하이드로볼의 비율이 높아질수록 해송, 장수매는 생존율과 생체중의 증가율이 높게 나타났고 맥반석의 비율이 높아질수록 진백, 목서의 생존율과 생체중은 높았다.

• 지구물리
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• 제7권2호
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• pp.113-120
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• 2004

Hydrochemical characteristics of deep groundwater at Surak-ri, Nonsan-gun, Chungnam Province was explained by major ion concentration, water type, and phase stability diagram. The area is composed of meta-sedimentary rock and quartz pophyry. The 5 boreholes where deep groundwater was sampled and analyzed are located on the meta-sedimentary rocks and drilling depth range of the wells is from 554 m to 928 m. pH, TDS, Na, and SiO2 values are high in the groundwater from meta-sedimentary area intruded by quartz pophyry, while Ca is high in the groundwater from meta-sedimentary area. K and Mg concentrations are low but F concentration is high both groundwater. The content of major anions is in the order of CO3(HCO3)>Cl>SO4(F) in both geology, while that of major cations shows the order of Na>Ca>K(Mg) in meta-sedimentary area intruded by quartz porphyry and a>Na>Mg>Na in meta-sedimentary area. Based on the phase equilibrium in the systems Na2O-Al2O3-SiO2-H2O and K2O-Al2O3-SiO2-H2O, the groundwater is saturated with respect to Quartz and more evolved compared with the natural mineral water. It is concluded that chemical evolution in the groundwater from meta-sedimentary area intruded by quartz porphyry, is nearly saturated with respect to feldspar, while the groundwater from meta-sedimentary area continue to proceed with increasing pH by reaction of feldspar.

• 자원환경지질
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• 제21권4호
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• pp.389-400
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• 1988

Minor elements such as Ag, As, Au, Bi, Cd, Cu, Co, Ni, Pb, Rb, Sb, Sr and Te were analyzed by atomic absorption spectrophotometry and induced coupled plasma spectrophotometry in order to investigate pathfinders for gold in quartz porphyry, granite porphyry and vein materials in Jeonjuil gold - silver mine, and in altered biotite granites and vein materials in Dukum gold - silver mine. In Dukum gold - silver mine, it is observed that Au contents have positive relation with As, Co, and Rb contents, but negative relation with Bi contents in altered biotite granites. Au contents have positive relation with Ag, As, Co and Te contents in vein materials. In Jeonjuil gold - silver mine, it is observed that Cd, Rb, Sr and Te are enriched near ore vein in quartz porphyry and granite porphyry. Au contents have positive relation with As, Cd, Cu, $Fe_2O_3$ and $K_2O$ in vein materials.

• 자원환경지질
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• 제17권1호
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• pp.17-34
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• 1984

어상천 망간광상은 조선계 홍훨리층의 돌로마이트와 삼태산층의 석회암내에 발달한 단층 파쇄대를 따라 형성된 표성산화망간광상이다. 본 산화망간광상의 하부에는 백악기 석영반암에 의하여 형성된 열수교대 내지 충진광상이 본 단충파쇄대를 따라 발달한다. 석영반암은 주성분으로 부터 계산한 노음치를 Q-K-F-PI 삼각도에 점시하면 북서단은 화강섬록암의 영역에 그리고 주암체는 화강암의 영역에 점시되고 D.I.치는 상기 북서단에서 부터 주암체쪽으로 증가한다. 따라서 이것은 마그마의 분화작용과 관계되는 것으로 보인다. 본 석영반암내 암질의 차이는 미량성분에도 반영이 되어 나타나고 있는 데 북서단에서 아연, 닉켈, 크롬, 몰리브텐의 함량이 높고 주암체에서는 동, 연의 함량이 높은 현상은 산성암과 염기성암에서 일반적으로 볼 수 있는 함량의 변화와 일치한다. 경상분지내 백악기 화강암류와 비교해 보면 동, 연, 아연, 닉켈, 크롬의 함량은 석영반암쪽이 분지내 동광상구의 화강암류보다 낮으나 동과 닉켈의 함량은 연 아연 광상구의 화강암류보다도 높은 경향을 보인다. 석회암 및 돌로마이트로 구성된 모암은 석영반암에 의한 광화작용으로 단층파쇄대에서는 망간, 연, 아연, 동등의 함량이 현저히 높고 멀어짐에 따라 감소되는 일차후생분산형태를 보인다. 토양중 미량원소의 함량은 토양의 생성조건 및 물리화학적조건과 밀접한 관계를 보이며 모암에서의 그들이 형성하는 탄산염의 용해도와도 주목할만한 관계를 보인다. 즉 난용성의 탄산염을 형성하는 미량원소는 토양중의 함량도 낮은 경향을 보인다.

• 한국축산시설환경학회지
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• 제5권3호
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• pp.157-170
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• 1999

This study was conducted to investigate the effects of Scoria, Quartz porphyry and Oak charcoal powder feeding by 1% level of concentrate on the fattening cross bred bulls(5/8 Korean Native Cattle, 2/8 Charolais, 1/8 Brahman germ plasma) Feeding trial was conducted with 4 treatment groups which were T1(Full feeding of concentrate and roughage for 12 months), T2(T1 and Scoria addition), T3(T1 and Quartz porphyry addition) and T4(Oak charcoal addition) for 360 days, consisting of 32 heads whose initially weights were about 299.7kg. The results obtained are summarized as follows; 1. During the over-all period, average daily gains by T3, T4, T2 and T1 were 1.024, 0.987, 0.977kg and 0.964, respectively, without a significant difference by treatments. 2. Concentrate intakes per body weight and TDN intakes required per unit of kilogram gain were lower in addition agent groups than in control, and in all the treatments feed efficiency was higher at early stage for 360 fattening day than at end stage. 3. Carcass weight, dressing percent, back-fat thickness and loin eye muscle area by treatments were 330.9 to 348.4kg(average 340.3kg), 55.2~56.2(average 55.8%), 0.41~0.55(average 0.46cm)and 76.0~80.9$\textrm{cm}^2$(average 77.6$\textrm{cm}^2$), respectively, and were improved in addition agent groups than in control. 4. Meat quality grade is higher in addition agent groups than in control, and heads of 1st grade by treatments was 3, 2, 1 and none in T4, T2, T3 and T1, respectively. 5. Incidence heads of diseases by treatment were not apparently different, but diseases of digestive system was decreased in addition agent groups than in control. 6. The nitrate nitrogen content of fattening bull dung which collected in rectum were 0.082~0.089% (average 0.084%), and the content in addition agent groups was smaller than in controll. 7. Income was higher in order of T4, T3, T2, and T1 and incomes of treatment groups were grater than that of control group by 21.4 to 33.5 percent. According to the above results it may be concluded that fattening bulls may be required to feed no more than 1% of Scoria, Quartz porphyry and Oak charcoal powder based on the concentrate feeding level during the fattening period(12 to 24 month of age) to produce high quality meat and increase income.

• 자원환경지질
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• 제19권spc호
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• pp.175-191
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• 1986

The Geodo granodiorite intruded into the Joseon Supergroup is fine-grained at the marginal part, and medium-grained and more leucocratic at the central part. The Quartz monzonite porphyry intruded inte Precambrian granite and Geodo granodiorite has abundant plagioclase phenocryst. The Imog granite intruded into the Yulri Group and the Joseon Supergroup is mediumgrained biotite granite with partly pinkish feldspar phenocryst. The K/Ar ages obtained from the biotite of the Geodo granodiorite and Imog granite are Early ($111{\pm}1{\sim}107{\pm}1$ Ma) and Late ($93{\pm}1{\sim}92{\pm}1$ Ma) Cretaceous, respectively. The K/Ar sericite age of the quartz-sericite zone of the lower Jangsan quartzite occuring in the western area gave much younger age (about 170 Ma) than that of the Jangsan quartzite, that might be reset due to the regional metamorphism of the Daebo orogeny. The granitic rocks of the area are felsic to mafic, metaluminous to peraluminous, calc-alkalic (alkali-lime index${\fallingdotseq}$ 57) and I-type (magnetite-series) based on the chemical data_ And they appear to have been fractionated at the order of Geodo granodiorite, Quartz monzonite porphyry and Imog granite. In terms of mineralogy, geochemistry and K/Ar biotite age, a rock suite of monzodiorite, quartz monzodiorite and quartz monzonite-granodiorite in the Geodo stock was fractionally differentiated from a magmatic body from its margin to inward.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 1998년도 가을 학술발표회 논문집
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• pp.313-318
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• 1998

• 자원환경지질
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• 제16권4호
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• pp.245-251
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• 1983

The Tongyeong gold-silver deposits is located in Chungmu City, the southern end of Korean peninsula. The ore deposits is epithermal gold-silver vein emplaced in late Cretaceous andesite, andesitic pyroclastics and quartz porphyry. Ore is composed of pyrite, chalcopyrite, sphalerite, galena, electrum, argentian tetrahedrite, Cu-Ag-sulfides, quartz and rhodochrosite. Filling temperature of fluid inclusions in quartz ranges from 134 to $223^{\circ}C$ and salinity ranges from 1.2 to 3.8 weight % equivalent to NaCl.

• 자원환경지질
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• 제18권1호
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• pp.11-22
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• 1985

The Daehwa and Donsan tungsten-molybdenum deposits are composed of numerous fissure-filling veins developed in Precambrian gneiss and Cretaceous granite and quartz porphyry. K-Ar age of biotite in granite and that of muscovite in ore veins are $105{\pm}5\;Ma$ and 88.2~88.6 Ma respectively. Occurrence of ore deposits shows that relevant igneous rock is possibly quartz porphyry rather than above mentioned granite in temporal view point. Vein structure and mineralogy suggest that ore veins were formed by continuous vein filling, not by repeated mineralization. Three distinct depositional stages with decreasing age can be devided on the basis of mineral paragenesis and fluid inclusion studies: Stage I, deposition of oxides and silicates; stage II, deposition of base-metal sulfides and sulfosalts with carbonates; stage III, deposition of barren calcite and fluorite. Tungsten, molybdenum and tin mineralization occurred in stage I.