• 암석학회지
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• 제6권1호
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• pp.19-33
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• 1997

본역의 지질은 백악기 경상누층군의 퇴적암, 이를 관입 또는 분출한 중성화산암류, 산성화산암류 및 제 4기 충적층으로 구성된다. 중성화산암류는 화성쇄설화산각력암, 석질화산력응회암, 안산암용암으로 구성되며, 산성화산암류는 데사이트질용결응회암 및 유문암용암, 유문암질응회암으로 구성된다. 본 연구에서는 중성 및 산성 화산암류에 대해 암석기재학적 연구와 신선한 시료 10개에 대한 암석화학적 특성을 고찰하고, K-Ar법에 의한 절대연대 측정을 실시하였다. 현미경 관찰에서 안산암용암은 사장석이 주 반정광물로 나타나며, 기질은 미정질 내지 은미정질로서 반정광물과 동일한 필로택시틱 조직을 보인다. 안산암질각력암은 퇴적암 및 안산암의 자력 암편을 포함한다. 테사이트질용결응회암은 현저한 파라택시틱 조직을 보이며, 유문암용암은 유상구조를 잘 보여 주고, 안산암의 암편을 함유하고 용결구조가 현저한 화산력용결응회암이 나타나는데, 유문암용암에서 기질의 함량은 80.9~ 89.3%에 이른다. 주 반정광물은 사장석이며 부분적으로 녹염석, 녹니석, 방해석, 제오라이트, 푸로필라이트 등으로 2차 변질되어 나타난다. 본역의 화산암류는 Norm값에 의한 Q-A-P 도표에서 현무암질안산암, 안산암, 데사이트, 유문암의 일련의 분화과정을 나타내고 대부눈 칼크알칼리 계열에 속한다. 화산암류의 화학조성은 $SiO_2$ 함량이 57.61~75.40 %이며, MgO, CaO, $Fe_2O_3$, $Al_2O_3$, $Ti_2$, MnO, $P_2O_5$ 등은 $SiO_2$함량이 증가함에 따라 연속적으로 증가하는 경향을 보인다. 주성분원소 및 미량 원소의 변화도에서 안산암질에서 유문암으로 분화되는, 즉 마그마의 정출 분화 특징을 뚜렷이 보여준다. REE 양상 및 spider 도표에서 일정한 분화 경향을 보이며 나란하다. spider 도표에서 본역의 화산암류는 Th, La, Nd, Gd 등이 부화되어 있으며, Ba, Nb, Sr, Hf, Zr 등이 결핍되어 있는 특징을 나타낸다. 안산암에서 유문암으로 분화가 진행될수록 Cs, Sr, Eu이 점차 결핍되는 경향이, Th가 증가하는 경향이 있고, Ba, Nb, Sr, Eu의 부(-)의 이상값이 점차 커지는 경향을 보인다. 희유 원소의 변화 경향에서 안산암과 중성 암맥, 데사이트와 유문암의 경향이 서로 일치함을 볼 수 있다. 주성분 원소 및 미량 원소 함량 변화는 본역의 화산암이 안산암으로부터 일연의 분별결정작용 산물임을 암시하며, 또한 $Al_2O_3$와 CaO 함량의 관계도, Th/Yb 비에 대한 Ta/Yb 비의 관계도, $Ce_N/Yb_N$ 대 $Ce_N$의 관계도에 따른 판별에서도 분별결정작용의 경향을 따르고 있다. 본역의 화산암은 $K_2O$, $Na_2O$, CaO 삼각도에서 도호의 영역에, Ba/La비, La/Th비에 의한 판별도에서 조산대의 high-K suite에 속한다. Rb 대 (Y+Nb)의 판별도 및 Hf-Th-Ta 지구조 판별도에서 지판이 침강 섭입하는 지판 경계부(destructive plate margin) 중 화산호의 조구적 영역에 도시된다. 본역의 화산암을 생성시킨 마그마는 $Al_2O_3$와 CaO 함량의 관계도, mode에서 나타나는 사장석 반정, 분화가 진행될수록 부의 Eu 이상이 증가하는 것 등에서 사장석의 분별이 우세한 분별결정작용을 거쳤음을 알 수 있다. 안산암질암을 관입한 중상 암맥에서 측정한 암석 년령은 $97.0{\pm}6.8~94.5{\pm}6.6$, 데사이트질암은 $68.9{\pm}4.8,\61.5{\pm}4.9~60.7{\pm}4.2$Ma으로 측정되었고, 이것은 백악기 유천층군과 대비되며, 백악기 유천층군 암석의 지화학적 자료와 본역 화산암의 지화하적 자료는 판별도 등에서 같은 영역에 도시된다.

• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 2008년도 추계학술대회 논문집 Vol.21
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• pp.200-200
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• 2008

This paper reports on electrical characterization by IDC pattern using BST$(Ba_{0.5}Sr_{0.5}TiO_3)$ thin film. BST thin films have been deposited on $Al_2O_3$ Substrates by Nd-YAG pulsed laser deposition with a 355nm wavelength at $700^{\circ}C$. The post deposition annealing at $750^{\circ}C$ in flowing $O_2$ atmosphere for I hours. The capacitance of IDC patterns have been measured from 1 to 10 GHz as a function fo electric field (${\pm}40$ KV/cm) at room temperature using interdiigitated Au electrodes deposited on top of BST. The IDC patterns have three type of fingers number. For the finger paris was increased onto $Al_2O_3$, the capacitance increased. The capacitance of 5 pairs finger was 0.3pF and 10 pairs finger was 0.9pF.

• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 2009년도 하계학술대회 논문집
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• pp.179-179
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• 2009

This is for the electrical characterization by IDC pattern using BST$(Ba_{0.5}Sr_{0.5}TiO_3)$ thin film. BST materials had been chosen for high frequency applications due to it's high permitivity and tunability. The BST thin films have been deposited on $Al_2O_3$ Substrates by Nd-YAG pulsed laser deposition with a 355nm wavelength at $700\;^{\circ}C$. The post deposition annealing at $750^{\circ}C$ in flowing $O_2$ atmosphere for 1 hours. The capacitance of IDC patterns have been measured from 1 to 10 GHz as a function of electric field ($\pm40$ KV/cm) at room temperature using inter-digital Au electrodes deposited on top of BST. The IDC patterns have three type of fingers number. For the 10 pairs finger was the best capacitance onto $Al_2O_3$ substrate. The capacitance was 0.9pF. Also Dielectric constant was been 351 at 100 mTorr and annealing temperature $750^{\circ}C$ for 1 hour. The loss tangent was been 0.00531.

• 한국지구과학회:학술대회논문집
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• 한국지구과학회 2005년도 추계학술발표회 논문집
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• pp.136-141
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• 2005

The K Ar ages, whole rock geochemistry and Sr Nd Pb isotopes have been determined for the submarine basalts dredged from the P2 and P3 segments of the Antarctic-Phoenix Ridge (APR), Drake Passage, Antarctica, for better understanding on temporal variation of magma chemistry in association with extinction of seafloor spreading. The fossilized APR is distant from the known hot spots, and consists of older N-MORB prior to extinction of spreading and younger E-MORB after extinction. The older N-MORB (3.5-6.4 Ma) occur in the southeast flank of the P3 segment (PR3) and the younger E-MORB (1.4-3.1 Ma) comprise a huge seamount at the P3 segment (SPR) and a big volcanic edifice at the P2 segment (PR2). The N-type PR3 basalts have higher Mg#, K/Ba, and CaO/Al2O3 and lower Zr/Y, Sr, and Na8.0 with slight enrichment in incompatible elements and almost flat REE patterns. The E-type SPR and PR2 basalts are highly enriched in incompatible elements and LREE. The extinction of spreading occurring at 3.3 Ma seems to have led to a temporal magma oversupply with E-MORB signatures. Geochemical signatures such as Ba/TiO2, Ba/La, and Sm/La suggest heterogeneity of upper mantle and formation of E-MORB by higher contribution of enriched materials to mantle melting, compared to N-MORB environment. E-MORB magmas beneath the APR seem to have been produced by low melting degree (up to 1% or more) at deeper low-temperature regime, where metasomatized veins consisting of pyroxenites have preferentially participated in the melting. The occurrence of E-MORB at the APR is a good example to better understand what kinds of magmatism would occur in association with extinction of spreading.

• 한국초전도ㆍ저온공학회논문지
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• 제8권4호
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• pp.15-18
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• 2006

REBCO coated conductors (RE: rare earth elements) have recently drawn great attention since they are known to possess stronger flux pinning centers in high magnetic fields compared with YBCO coated conductors. In this study, $GdBa_2Cu_3O_{7-d}(GdBCO)$ was selected to investigate the influence of the distance between target and substrate and substrate temperature on the superconducting properties of GdBCO films on the $SrTiO_3(100)$ substrate. Samples were fabricated by pulsed laser deposition (PLD) with a Nd:YAG laser (355nm). Under a given oxygen pressure of 800mTorr, we changed the distance between target and substrate from 5.5cm to 7.0cm and the substrate temperature from $750^{\circ}C\;to\;850^{\circ}C$. The crystallinity and texture of GdBCO films were analyzed by X-ray diffraction (XRD), and the surface morphology was observed by the scanning electron microscopy (SEM). Tc and Jc values were measured by the four point probe method. High quality GdBCO films with Tc of 89.7K and Jc over $1MA/cm^2$ at 77 K in self field were successfully fabricated by optimizing processing parameters. The detailed processing conditions, microstructure and superconducting properties will be presented for a discussion.

• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 2008년도 추계학술대회 논문집 Vol.21
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• pp.79-79
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• 2008

We report the growth of $Ba_{0.5}Sr_{0.5}TiO_3$(BST) thin films and their substrate-dependent electrical characteristics. BST thin films were deposited on alumina(non-single crystal), $Al_2O_3$(100) substrates by Nd:YAG Pulsed Laser Deposition(PLD) with a 355nm wavelength at substrate temperature of $700^{\circ}C$ and post-deposition annealing at $750^{\circ}C$ in flowing $O_2$ atmosphere for 1hours. BST materials had been chosen due to high dielectric permittivity and tunability for high frequency applications, To analyze the oxygen partial pressure effects, deposited films at 1, 10, 50, 100, 150, 200, 300 mTorr. The effects of oxygen pressure on structural properties of the deposited films have been investigated by X-ray diffraction(XRD) and atomic force microscope(AFM), respectively. Then we manufactured a inter-digital capacitor(IDC) patterns twenty fingers and $10{\mu}m$ gap, $700{\mu}m$ length and electrical properties were characterized. The results provide a basis for understanding the growth mechanisms and basic structural and electrical properties of BST thin films as required for tunable microwave devices applications such as varactors and tunable filters.

• Progress in Superconductivity
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• 제5권1호
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• pp.50-54
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• 2003

We have fabricated $∂^2$$B_{z}$ /$∂x^2$ type planar gradiometers and studied their properties in operation under various field conditions. $YBa_2$$Cu_3$$O_{7}$ film was deposited on $SrTiO_3$ (100) substrate by a pulsed laser deposition (PLD) system and patterned into a device by the photolithography with ion milling technique. The device consists of 3 pickup loops designed symmetrically Inner dimension and the width of the square side loops are 3.6 mm and 1.2 mm, respectively, and the corresponding dimensions of the center loop are 2.0 mm and 1.13 mm. The length of baseline gradiometer is 5.8 mm. Step-edge junction width is 3.0 $\mu\textrm{m}$ and the hole size of the SQUID loop is 3 $\mu\textrm{m}$ ${\times}$ 52 $\mu\textrm{m}$. The SQUID inductance is estimated to be 35 pH. The device was formed on a 20 mm ${\times}$ 10 mm substrate. We have tested the behavior of the device in various field conditions. The unshielded gradiometer was stable under extremely hostile conditions on a laboratory bench. Noise level 0.45 pT/$\textrm{cm}^2$/(equation omitted)Hz and 0.84 pT/$\textrm{cm}^2$/(equation omitted)Hz at 1 Hz for the shielded and the unshielded cases, which correspond to equivalent field noises of 150 fT/(equation omitted)Hz and 280 fT/(equation omitted)Hz, respectively. In spite of the short baseline of 5.8 mm, the high common-mode-rejection-ratio of the gradiometer, $10^3$, allowed us to successfully record magnetocardiogram of a human subject, which demonstrates the feasibility of the design in biomagnetic studies.

• 자원환경지질
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• 제56권3호
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• pp.259-275
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• 2023

Pan African granitoids of Kaiama is comprised of K-feldspar rich granites, porphyritic granites, and granitic gneiss that are intruded by quartz veins and aplitic veins and dykes which trend NE-SW. In order to establish the geochemical signatures, petrogenesis, and tectonic settings of the lithological units, petrological, petrographical, and geochemical studies was carried out. Petrographic analysis reveals that the granitoids are dominantly composed of quartz, plagioclase feldspar, biotite, and k-feldspar with occasional muscovites, sericite, and opaque minerals that constitute very low proportion. Major, trace, and rare earth elements geochemical data reveal that the rocks have moderate to high silica (SiO₂=63-79.7%) and alumina (Al₂O₃=11.85-16.15) contents that correlate with the abundance of quartz, feldspars, and biotite. The rocks are calc-alkaline, peraluminous (ASI=1.0-<1.2), and S-type granitoids sourced by melting of pre-existing metasedimentary or sedimentary rocks containing Al, Na, and K oxides. They plot dominantly in the WPG and VAG fields suggesting emplacement in a post-collisional tectonic setting. On a multi-element variation diagram, the granitoids show depletion in Ba, K, P, Rb, and Ti while enrichment was observed for Th, U, Nd, Pb and Sm. Their rare-earth elements pattern is characterized by moderate fractionation ((La/Yb)_N=0.52-38.24) and pronounced negative Eu-anomaly (Eu/Eu^*=0.02-1.22) that points to the preservation of plagioclase from the source magma. Generally, the geochemical features of the granitoids show that they were derived by the partial melting of crustal rocks with some input from greywacke and pelitic materials in a typical post-collisional tectonic setting.