• Transactions on Electrical and Electronic Materials
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• v.2 no.4
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• pp.11-14
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• 2001

Phase intergrowth in BSCCO thin films has been Investigated. It turfed out from XRD analyses of these phases that molar fraction of each constituent phase in the intergrowth thin film can be exhibited as a function of substrate temperature and ozone pressure. Super- conducting behavior of the intergrowth thin aim Is also discussed.

• Journal of the Mineralogical Society of Korea
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• v.12 no.2
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• pp.66-76
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• 1999

Intergrowth texture of biotite and chlorite crystals within an amphibolitic schist of the northwestern Okchon metamorphic belt was investigated using back-scattered electron (BSE) imaging and high-resolution transmission electron microscopy (HRTEM). BSE images show that thin chlorite and biotite packets are mixed along (001) plane to result in intergrowth texture. In addition, rutile particles of submicron size occur exclusively at the boundaries between biotite and chlorite stacks. HRTEM investigation and remnant biotite layers are closely associated with such boundaries, suggestinga possibility that chlorite layers were formed from biotite during retrograde metamorphic reaction. Such intepretation of the origin of intergrowth texture can be further supported biotite is approximately 2 w%, and that of chlorite usually lower than 0.2 wt%. Ti was apparently leached out during the alteratin of biotite to precipitate rutile particles at the such rutile particles could be an important indicator showing that the intergrowth texture of chlorite and biotite is originated by a retrograde metamorphism rather than by incomplete chlorite-to-biotite reaction during prograde metamorphism. Biotite crystals contain intercalated chlorite layers will result in somewhat high Mg and Al, and the use of such inhomogeneous biotite will result in impreciese geothermobarometric calculations.

• Proceedings of the Korean Institute of Electrical and Electronic Material Engineers Conference
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• 2001.07a
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• pp.327-330
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• 2001

Phase intergrowth in BSCCO thin films have been investigated. It turned out from XRD analyses of these phases that molar fraction of each constituent phase in the intergrowth thin film can be exhibited as a function of substrate temperature and ozone pressure. Superconducting behavior of the intergrowth thin film is also discussed.

• Progress in Superconductivity and Cryogenics
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• v.24 no.4
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• pp.25-28
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• 2022

We investigated the formation of superconducting intergrowth phases through the interface reaction both between TlSr₂Cu₁O₅ (Tl-121) and (CrO₄)Sr₂CuO₂, and between Tl -121 and ((CO₃)_0.5(CrO₄)_0.5 Sr₂CuO₂ phases. We found oxychromate intergrowth phases can be formed through the interface reactions and a new superconducting oxychromate compound TlSr₄Cu₂O_z(CO₃)_0.5(CrO₄)_0.5 with T_c above 73 K was discovered based on the results of the interface reactions.

• Journal of the Mineralogical Society of Korea
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• v.8 no.1
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• pp.1-12
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• 1995

옥천 변성대 남서부 지역에서 산출되는 변성 니질암에서는 muscovite, biotite 및 chlorite를 주로하는 phyllosilicate가 서로 intergrowth 또는 interlayer를 이루는 것이 편광현미경 관찰, EPMA 분석, Back Scattered Electron (BSE) image 관찰 및 Transmission Electron Micro-scope(TEM) 관찰을 통하여 확인되었다. 이들 광물들은 편광현미경 관찰에서 흔히 각각의 입자를 식별할 수 없을 정도의 미세 규모로 서로 intergrow 되어 있으며BSE image에서는 0.1$\mu\textrm{m}$ 이하의 아주 작은 크기에서부터 10.0$\mu\textrm{m}$ 정도 크기까지 다양한 규모의 intergrow를 형성하고 있음이 관찰되었다. TEM scale에서는 개별 layer 크기(약 10$\AA$)에서부터 수십 개 layer 크기의 interlayering을 보여준다. 이와 같은 intergrowth 또는 interlayering의 결과로 EPMA 분석에서 종종 보기에는 규진(homogeneous)한 입자라 하더라도 두 개 이상의 광물 성분이 섞여 있는 분석값을 나타내며 이러한 nonstoichiometry는 BSE image에서 interlayer(또는 intergrow) 된 것으로 관찰되는 부분에서 더욱 두드러진다.Chlorite zone에서는 chlorite와 muscovite의 interlayering (C/M)이 주로 발견되며 biotite zone과 garnet zone에서는 chlorite와 biotite의 interlayer (C/B)가 주로 관찰된다. 이는 chlorite zone에서는 속성작용에서 보편적으로 나타나는 C/M으로부터 chlorite가 분리되는 광물반응이 일어나는데 반해서 biotite zone과 garnet zone에서는 chlorite로부터 C/B를 거쳐 biotite를 생성하는 광물반응이 일어나는 것을 의미한다. 이와 같은 현상은 변성작용에서 phollosilicate의 광물반응의 엄밀한 의미에서는 평형(equilibrium) 상태에서 균질한 광물을 생성하기보다는 비평형(disequilibrium) 반응으로 일어난다는 것을 의미한다.

• Journal of the Korean Institute of Electrical and Electronic Material Engineers
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• v.15 no.8
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• pp.736-741
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• 2002

Phase intergrowth some kinds of the $Bi_2Sr_2Ca_{n-1}Cu_nO_y$ phases is observed in the thin film fabrication at ultralow co-deposition with multi targets by means of ion beam sputtering. The molar fraction of the Bi2212 phase in the mixed crystal of the grown films is investigated as a function of the applied ozone pressure and the substrate temperature. The activation energy for the phase transformation from the Bi2201 to the Bi2212 is estimated in terms of the Avrami equation. This study reveals that the formation of a liquid phase contributes significantly to the construction of the Bi2212 phase in the thin films, differing from the bulk synthesis.

• Proceedings of the Korean Institute of Electrical and Electronic Material Engineers Conference
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• 2002.07a
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• pp.490-493
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• 2002

Phase intergrowth some kinds of the Bi$_2$Sr$_2$Ca$\_$n-1/Cu$\_$n/O$\_$y/ phases is observed in the thin film fabrication at ultralow co-deposition with multi targets by means of ion beam sputtering. The molar fraction of the Bi2212 phase in the mixed crystal of the grown films is investigated as a function of the applied ozone pressure and the substrate temperature. The activation energy for the phase transformation from the Bi2201 to the Bi2212 is estimated in terms of the Avrami equation. This study reveals that the formation of a liquid phase contributes significantly to the construction of the Bi2212 phase in the thin films, differing from the bulk synthesis.

• Journal of the Mineralogical Society of Korea
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• v.15 no.2
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• pp.122-131
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• 2002

Muscovite, chlorite and biotite in metapelites of the Ogcheon Hetamorphic Belt are studied using electron probe microanalysis (EPMA), backscattered electron images (BEI) of scanning electron microscopy (SEM) and lattice fringe images of transmission electron microscopy (TEM). These minerals are observed to be intergrown under a polarized light microscope and are apparently interlayered below EPMA resolution; EPMA data often indicate mixtures of phyllosilicates such as muscovite/chlorite (M/C), biotite/chlorite (B/C), muscovite/pyrophyllite/chlorite (M/P/C). biotite/pyrophyllite/chlorite (B/P/C) or biotite/muscovite/chlorite (B/M/C). BEI observations show that the three minerals (muscovite, chlorite and biotite) are mixed at various scales in a grain through the garnet zone, and the interlayering of the three minerals are observed from TEM lattice fringe images and selected area electron diffraction patterns. The result of TEM observations reveals that 7-$\AA$ layers (serpentine, precursor of chlorite) are interlayered within 10-$\AA$ layers (muscovite) at 100~200 $\AA$ scale as well as M/C in the chlorite zone. The 7-$\AA$ layers become smaller in size and less frequent in the biotite tone, and 10-$\AA$ layers are interlayered with chlorite (14 $\AA$) at an individual layer scale. The 7-$\AA$ layers are no longer observed in the garnet zone, and 10-$\AA$ layers (biotite) are interlayered with chlorite (B/C) at 50~100 $\AA$ scale. Relatively large scale (1000~2000 $\AA$) of intergrowth is also frequently observed from the garnet zone samples. However, rocks from all three metamorphic zones show interlayering of a few units of 7-, 10- and 14-$\AA$ layers with each other at TEM observations. The result of this study implies that metamorphic minerals such as muscovite, chlorite and biotite form through disequilibrum mineral reactions resulting in inhomogenious phases.

• Transactions on Electrical and Electronic Materials
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• v.5 no.5
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• pp.199-203
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• 2004

Superconducting B $i_2$S $r_2$C $a_{n-l}$C $u_{n}$ $O_{x}$(n=2～4) thin films were prepared by single target DC-magnetron sputtering. And, that was compared with the B $i_2$S $r_2$C $a_{n-l}$C $u_{n}$ $O_{x}$(n=1～3) thin film fabricated by using the ion beam sputtering. Phase intergrowth among n=2-3, 3-4 and 4-5 phases was observed. The molar fraction of each phase in the mixed crystal of the deposited films was determined by x-ray diffraction analyses and investigated as a function of $O_2$ gas pressure during sputtering. We investigated the changes of the superconducting properties by molar fraction of each phase. Also, the thin film surface observation was carried out by atomic force microscope. The images show the average particle size decreases, and the distribution density of particles on the film surface was to increase with lower gas pressures. The fabrication conditions for selective growth of the single n=2, 3 and 4 phases in BiSrC $a_{n-l}$C $u_{n}$ $O_{x}$(n=2～4) thin film are discussed.e discussed.ussed.

• 한국전자현미경학회:학술대회논문집
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• 1994.05a
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• pp.31-31
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• 1994