삼기층(三紀層)에 배태(胚胎)된 벤토나이트의 산소(酸素) 및 수소동위원소(水素同位元素) 연구(硏究)

문희수,Moon, Hi-Soo 대한자원환경지질학회 1986 자원환경지질 Vol.19 No.no.spc

Hydrogen and oxygen isotope ratios of thirteen of the under 2 micron size fraction of the montmorillonites were measured. The oxygen isotopic compositions of these samples range from + 17.0 to +25.1 permil and the hydrogen isotope compositions range from -47.5 to -65.8 permil with an average standard deviation of 0.7 and 2.7 permil, respectively. The oxygen isotope compositions show a positive relationship with stratigraphy whereas the hydrogen isotope compositions do not. It suggest that the montmorillonite attained isotopic equilibrium at the maximum burial depth and ratained their oxygen isotope composition on subsequent uplift. Possibilities of montmorillonite formation by weathering or hydrothermal alteration of volcanic material are eliminated by the ${\delta}D$ and ${\delta}^{18}O$ values of these samples. Calculated formation temperature lie between 29 to $80^{\circ}C$.

질석화가 진행된 풍화단면에서의 광물조성과 주원소의 변화

문희수,송윤구,신상은,Moon, Hi-Soo,Song, Yungoo,Sin, Sang Eun 대한자원환경지질학회 1993 자원환경지질 Vol.26 No.1

Several vermiculite deposits occur as the alteration product from phlogopite in ultramafic rock, in the Hongseong and Cheongyang area, South Korea. Some quarries show well-defined weathering profile. Samples collected from those quarries were examined by XRD and chemistry to define a vertical variations in mineralogy and chemistry of the weathering profile developed on ultramafic rocks. The analysis by X-ray diffractometry showed that mineral compositions changed continuously as depth of profile increasing, the vermiculite-the phlogopite/vermiculite interstratified-the phlogopite. Chemical analysis of bulk samples in altered zone revealed that regardless of composition and kinds of mineral in the rock, there are significant increase of MgO, CaO and $H_2O$, and decrease of K as depth of profile decrease reflecting the characteristics in vermiculitization. Also, there was a tendency that weathering indicies of each sample horizon change gradually with increasing depth. This tendency can be explained as variations of degree of vermiculitization. The regular changes of mineralogical and chemical composition in vertical profile suggest that weathering is the most important process in vermiculitization in this area.

국내산(國內産) 벤토나이트의 몇 가지 물리화학적(物理化學的) 특성(特性)에 관(關)하여

문희수,유장한,김종환,조한익,Moon, Hi-Soo,You, Jang Han,Kim, Jong Hwan,Cho, Han Ik 대한자원환경지질학회 1987 자원환경지질 Vol.20 No.3

Some physico-chemical properties such as surface area, moisture content, cation exchange capacity, swelling rate, pH, viscosity and liquid limit have been determined for evaluation of Cabentonite deposit occurring in four localities; Yonil, Gampo, Haseo and Pohang, in Gyeongsang-do. Montmorillonite contents can be derived from surface area measurement. Enhancement of liquid limit values and swelling volume were observed in the samples which had higher exchangeable Na ion and finer particle-size distribution. Identical results were observed even in the Na-exchanged samples. This suggests that aggregation effects have a great influence on physico-chemical properties. Aggregation of montmorillonite were controlled not only burial depth but also composition of exchangeable cation. Consequently, sample occurred in Yonil area where has the greatest burial depth in the area show somewhat lower physico-chemical properties than those of samples occurred in the other localities. However, the basic test applied in this study provides very useful preliminary information relating to its commercial potential.

강화도(江華島) 온수리(溫水里) 지역(地域) 화강암(花崗岩)의 풍화작용(風化作用)에 의한 카올리나이트의 형성(形成)

문희수,김신애,Moon, Hi-Soo,Kim, Shin Ae 대한자원환경지질학회 1989 자원환경지질 Vol.22 No.1

Strongly weathered granitic rocks are widely distributed in the south-eastern part of the Ganghwa island. Kaolinite developed during intense weathering on this granitic rocks have been studied mineralogically and chemically. Various weathering indexes were ca1culated on the basis of oxide. Those indexes are slightly varied with depth. It shows that the percentages of $Al_2O_3$ increase but that of $CaO+Na_2O+K_2O$ decrease as the weathering progress. These results indicate that day minerals, mainly kaolinite with the appreciable amount of halloysite, were formed by the weathering of feldspars in the granitic rocks. X-ray diffraction, differential thermal analysis, infrared spectrometry and electron microscopy were used to characterize and estimate crystallinity of the kaolinite. Generally, Kaolinite shows a less sharp basal reflection and relatively low dehydroxylation temperature, indicating disordered kaolinite. They usually occur aggregates as a vermicular kaolinites showing loose basal plane stacking arrangement.

동양활석광상(東洋滑石鑛床)에서 산출(産出)되는 활석(滑石)에 대한 광물화학적(鑛物化學的) 및 성인적(成因的) 연구(硏究)

문희수,김성태,Moon, Hi-soo,Kim, Seong Tae 대한자원환경지질학회 1988 자원환경지질 Vol.21 No.3

Talc deposit of pipe-like form occurrs in the lower part of the Hyangsanri Dolomite with a strike of N40 -50 E and a dip of 40 -50 NW which is one formation of the Ogcheon Super Croup. The pipi-like ore body plunge at about $40^{\circ}$ to the west and are parallel to the lineation developed in the area. Structural formulae of tales occurred in this deposit are close to the ieal composition $Mg_6Si_8O_{20}(OH)_4$ showing limited deviation from ideal one. Substitution of Al for Si in tetrahedral site is of little or nothing ranging 0-0.04 and octahedral occupancy is close to six ranging 5.88-5.98 atoms per unit cell. Predominant octahedaral cation is Mg and proportion of divalent cations is generally over 97percent. Calcite -dolomite thermometry is obtained by determining the mol % $MgCO_3$using of EPMA and XRD methods. The peak metamorphic temperature can be estimated at $470{\pm}30^{\circ}C$ in the area whereas carbonates occurred at near talc ore show lower temperature than $400^{\circ}C$ that the calcite solvus limit is not well established. It indicates that the talc deposit was formed at the lower temperature that the metamorphic temperature. Cosequently, the formation of talc by metamorphism is questionable and the alteratin zone developed around the talc ore is very limited. The occurrence of talc ore in the dolomite as well as mineralogy, calcite-dolomite geothermometry, chlorite geothermometry, field and microscopic evidence suggest that siliceous ascending hydrothermal solution along the fracture is responsible for the formation of talc. It was considered that the slight fracturing of dolomite was formed by deformation prior to the mineralization.

Hydrothermal Alteration Related to Cretaceous Felsic Magmatism in the Gusi Mine, Southern Korea

문희수,노열,김인준,송윤구,이현구,Moon, Hi-Soo,Roh, Yul,Kim, In-Joon,Song, Yungoo,Lee, Hyun Koo The Korean Society of Economic and Environmental G 1991 자원환경지질 Vol.24 No.1

Gusi pyrophyllite deposit is located in the Haenam volcanic field in the southwestern part of the Korea Peninsula. This area is known for the occurrences of pyrophyllite, alunite and dickite. This volcanic field is composed of andesite, rhyolite and pyroclastic rocks of late Cretaceous age The pyroclastic rocks are hydrothermally altered to pyrophyllite and kaolin minerals forming the Gusi deposits. The hydrothermally altered rock can be classified into the following zones on the basis of their mineral assemblages: quartz, pyrophyllite, dickite and illite-smectite zones, from the centre to the margins of the alteration mass. Such mineral assemblages indicate that the country rocks, most of which are the lower Jagguri Tuff, were altered by strongly acidic hydrothermal solutions with high aqueous silica and potassium activity and that the formation temperature of pyrophyllite is higher than $265^{\circ}C$. The mechanism of the hydrothermal alteration is considered to be related to felsic magmatism. 구시납석광상은 전남 해남지역의 중생대 백악기 화산암류를 모암으로 산출된다. 모암을 이루는 화산암류는 대부분 웅회암류이나 일부 유문암의 변질산물도 있으며, 이들의 열수변질 산물로서 구시광상의 납석 및 도석을 형성 시켰다. 이 변질작용의 결과로 형성된 광물조합에 의하여 이들은 변질대의 중심부로부터 외각으로 가면서 납석, 디카이트, 석영 및 일라이트-스멕타이트대로 구분된다. 이러한 변질광물의 분포양상은 모암인 장구리응회암이 상대적으로 높은 Si와 K이온 활동도를 갖는 강한 산성 열수용액에 의한 변질작용에 의하여 형성되었음을 지시한다. 이들 광물의 안정영역을 고려할 때 일라이트-스멕타이트대는 $200^{\circ}C$ 이하에서, 디카이트대는 $200{\sim}250^{\circ}C$ 범위에서, 납석대는 $260^{\circ}C$ 이상의 온도 영역에서 형성 되었음을 지시한다. 납석대의 일부에서 다이아스포어를 함유하는 것으로 보아 이때의 최고 온도는 $300^{\circ}C$ 정도에 이르렀을 것이다. 이들 변질작용은 본역에 분포된 화산암류를 형성시킨 화산활동에 기인된 열수변질작용으로 해석된다.

감포지역(甘浦地域) Ca-몬모릴로나이트의 광물학적(鑛物學的) 및 열적특성(熱的特性) : 죽전(竹田) 및 용동리지역(龍洞里地域) 광상(鑛床) 비교연구(比較硏究)

문희수,안재영,최선경,김문영,디. 제이. 모간,Moon, Hi-Soo,Ahn, Jae Yeong,Choi, Sun Kyung,Kim, Moon Young,Morgan, D.J. 대한자원환경지질학회 1989 자원환경지질 Vol.22 No.3

Eight under 2 micron size fractions of the montmorillonite from Jugjeonri area, Gyeongsanbug-do, were studied and then this result has been compared with data from Yongdongri area. Montmorillonites occurring at the same stratigraphic horizon in each area show limited variation in chemical composition, but shows some degree of differences in exchangeable cation compositions and total layer charges of montmorillonites from Jugjeonri to Yongdongri area. In general, samples from Jugjeonri show higher amount of exchangeable Na and layer charge due to relatively higher substitution of Mg for Al in octahedral sites than those from Yongdongri area. But Their dehydroxylation endothermic peaks of the samples from both areas are abnormal type with a small range of variation of peak temperature. This variation seems to reflect tetrahedral substitution of AI for Si for samples from Yongdongri whereas samples from Jugjeonri do not show shuch a tendency. However, samples from Jugjeonri proved to be relatively higher dehydroxylation peak temperatures than those of the other. DSC data for sample from Jugjeonri also show that divalent-cation saturated montmorillonite have relatively a higher endothermic heat capacities than monovalent-cation saturated one as shown in previous work. Two different morphologies of montmorillonites, honeycomb structure and closely packed intergrowth, by SEM were observed in samples from both areas but the later one is common. The scalloped type is relatively abundant in the sample from Yongdongri than the other. The dominant habit by TEM are irregularly shaped foliated aggregates and platy shaped particles. In general, foliated aggregates which are easy to disperse are relatively abundant in the samples from Jugjeon compared with those from Yongdongri area.

Thermal Behaviour of Some Montmorillonites with related their Chemical Compositions

문희수,Moon, Hi-Soo The Korean Society of Economic and Environmental G 1985 자원환경지질 Vol.18 No.3

경상도 연일, 감포 및 하서지역의 삼기층에서 산출되는 13개 몬모릴로나이트에 대한 화학조성과 열적성질을 연구하였다. 이들의 화학조성으로부터 계산된 결정구조식은 사면체내의 $Si^{4+}$는 $Al^{3+}$에 의하여 단위격자당 0.02에서 0.33 원자가 치환되었으며 전체 층간부전하의 4~47%가 사면체내의 치환에서 유래되고 있다. 대부분의 시료는 85% 이상의 부전하는 팔면체내의 치환에 의해서 유래되고 있었다. 몬모릴로나이트의 결정구조식과 시차열 및 열천평곡선에 의한 열적특성 결과를 비교 검토한 결과 몬모릴로나이트의 팔면체내의 Al의 Fe에 의한 치환 및 사면체내의 Si의 Al에 의한 치환 모두가 dehydroxylation 온도를 감소시키는 결과를 초래했다. 이러한 관계는 금번 실험된 시료들에서는 충분한 정의 관계를 보였으나, 팔면체 및 사면체내에서의 치환정도가 현저히 다른 시료로서 연구한 결과가 이와 일치된다면 일반적인 현상으로 받아 들일 수 있을 것이다. Detailed chemical compositions of thirteen montmorillonites and their thermal behaviour by differential thermal and thermogravimetric analysis have been studied. Comparison of structural formulae with experimental results by thermal analysis gave evidence of that both substitutions of Fe for Al in octahedral and Al for Si in tetrahedral positions appear to affect dehydroxylation temperature, which is valid for the present samples. Further detailed study of this topic using well-known samples which have various degree of substitution will be justified.

전남 해남지역 해남 납석광상의 변질작용 및 생성환경

문희수,정승우,송윤구,박영석,Moon, Hi-Soo,Jeong, Seung Woo,Song, Yungoo,Park, Young Surk 대한자원환경지질학회 1991 자원환경지질 Vol.24 No.2

Haenam pyrophyllite deposit occurred in the rhyolitic tuff of late Cretaceous age is located in the northern part of Haenam-gun, Jeonranam-do. The ore of the Haenam deposit is predominantly composed of pyrophyllite and illite accompanying such clay minerals as kaolinite, chlorite, and smectite. Pyrophyllite ore at the center of altered mass is often associated with kaolin minerals and high temperature minerals such as corundum, andalusite, and diaspore. On the basis of mineral assemblage the Haenam deposit can be devided into three alteration zones from the center to the margin of the deposit; the pyrophyllite zone, kaolinite zone, and illite zone. All alteration zones are associated with appreciable amounts of chalcedonic quartz. Those mineral assemblages indicate that hydrothermal solution which produced the Haenam deposit is strongly acidic solution with high silica and hydrogen activity and low $SO_4{^{2-}}$ activity. Discriminant analysis shows that $Na_2O$, $K_2O$, and $Al_2O$, of major elements are discriminant elements which classify alteration zones, while in case of trace elements Cr, Ni, and Sr turned out to be discriminant elements in this deposit. According to the mineral assemblage and illite geothermometry, pyrophyllite ore is considered to have been formed at about $240-290^{\circ}C$. K-Ar isotopic age for illite from this deposit indicates that it was formed at much the same age of later stage volcanics in the area, suggesting that the hydrothermal alteration of these deposits is associated with later volcanism of the area.

Thermal and Mineralogical Characterization of Ca-Montmorillonite from Gampo Area

문희수,최선경,김문영,Moon, Hi-Soo,Choi, Sun Kyung,Kim, Moon Young The Korean Society of Economic and Environmental G 1988 자원환경지질 Vol.21 No.2

Ten under 2 micron size fractions of the montmorillonite from Yongdongri area, Gyeongsangbug-Do were studied using X-ray powder diffraction, cation exchange measurement, differential thermal analysis, thermogravimetric analysis, differential thermal scanning calorimetry and chemical analysis. Montmorillonites occurring at same deposit show limited variation in chemical composition whereas in thermal properties they do not. Their dehydroxylation endothermic peaks are "abnormal" type with a small range of variation of peak temperature reflecting tetrahedral substitution of Al for Si. Data from DSC show that divalent-cation saturated montmorillonite has relatively a higher endothermic heat capacity than monovalent-cation saturated montmorillonite, indicating that cations with higher electronegativity hold more water molecules. 감포지역(甘浦地域)의 용동리에서 용동리응회암(龍洞里凝灰岩)내에 배태되는 Ca-몬모릴로나이트들은 비록 동일층준(同一層準)에서 산출(産出)되나 제한적(制限的)이지만 화학조성(化學組成)의 차이(差異)가 나타난다. 이들의 열적특성은 "비정상형(型)"으로 나타나며, 탈수와 관계된 흡열반응피크의 온도(溫度)는 사면체내의 Si를 치환한 Al의 양적비에 따라 약간변화된다. 이러한 사실은 제한적인 화학조성의 변화는 열적특성에 큰 영향을 미치지 못함을 지시한다. 시차주사열량 측정결과 2가의 양이온으로 치환 된 시료의 경우 1가의 양이온으로 치환된 시료보다 흡열용량이 증가되는 경향을 보이므로 시료내의 우세한 양이온의 종류를 예상할 수 있으며, 전기음성도가 큰 이온일수록 더 많은 물분자를 취(取)함을 알수있다.