• 한국가스학회지
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• 제23권1호
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• pp.1-11
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• 2019

한국 정부는 액화 천연가스를 대체하는 에너지원으로서 러시아의 파이프라인 천연가스 도입을 1990년대 이후부터 지속적으로 모색해오고 있다. 이러한 동북아 에너지 협력에 대한 논의가 현실 정치뿐만 아니라 학술적인 차원에서도 다양하게 진행되고 있지만, 기존의 선행연구들은 협력의 당위성만을 제시하고 있을 뿐이지 이론적 분석틀이 미약하다는 한계를 지니고 있다. 이에 본 논문에서는 경제통합론이라는 이론적 자원을 바탕으로 에너지협력의 동기 조건 단계를 분석하고자 한다. 연구 결과 동북아 천연가스 협력과 관련해서는 경제적 동기만이 유일하기는 하지만, 실질적인 기대이익뿐만 아니라 경제구조의 보완성과 정책목표의 수렴성이라는 조건들이 갖추어진 것으로 파악되었다. 결론적으로 동북아에서 높은 수준의 에너지 협력은 어렵겠지만 특혜무역협정 수준의 초보적인 천연가스 협력이 가능하다는 전망이 제시될 수 있었다.

• 동남아시아연구
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• 제21권3호
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• pp.139-203
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• 2011

This paper attempts to review of recent development of ASEAN financial integration and to evaluate it and predict its future aspect. For this purpose, we first examine the historic aspect of ASEAN financial integration such as ASEAN financial service open agreement or ASEAN capital market forum report and currently agreed integration plan. In addition, we study the development stages of ASEAM member countries in terms of its economic size or income level. Finally, we look at the financial market and institutional aspect of ASEAN member countries and the recent development of global financial market. From these analyses, we find several important facts. First, it is true that ASEAN, in general, will enjoy the effect of expanding regional investment and improving the quality of financial service through the financial integration. We think that its long term benefit is too large for ASEAN member states to avoid. Second, as a result, it is certain that ASEAN will corporate further to make its financial market to be integrated in the future. Third, however, despite these benefits and continuing efforts, we expect that it will be very difficult for ASEAN to reach a stage of financial integration as suggested in the Blueprint of ASEAN Economic Community by the year of 2015. The large difference among member states in term of economic and financial development will not allow for them to reach a single goal within a short time. Instead, we expect the following scenario for the integration process will hold. First, ASEAN will reach an agreement on the institutional framework by 2015 and afterwards, slowly the markets will begin to integrate. Second, at the earlier stage, not all but some countries will start the integration process. We expect that the financial market of ASEAN 5 will first be integrated and other 5 will join to it later.

• 벤처창업연구
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• 제16권5호
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• pp.1-14
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• 2021

전 세계적으로 혁신과 창업기업의 스케일업이 중요한 국가적 과제로 부각되고 있다. 과거 경기침체 극복을 위해 'Start-tup America', 'Start-up Chile', 'Start-up Britain' 등 스타트업 중심의 정책 패러다임을 확산시켰다. 최근 창업선진국을 중심으로 경기회복이 가시화되면서, 스타트업 중심의 정책 패러다임이 'Scale-up America', Scale-up UK', 'Scale-up Denmark' 등 스케일업 중심의 정책 패러다임으로 전환하고 있는 추세이다. 창업기업은 스타트업 단계를 넘어서 스케일업 단계로 진입해야 국가적으로 양질의 일자리가 늘어나고 경제성장으로 나아갈 수 있다. 그러므로 창업기업을 강한 중견기업으로 성장시켜 지속적으로 생존할 수 있는 발판을 마련해주어야 한다. 이에 따라 본 연구는 창업기업이 스케일업 기업으로 성장할 수 있도록 성장의 선행변수인 성장 열망에 영향을 미치는 요인들을 심층적으로 고찰하고 국가의 경제발전단계 간, 기업가 간의 차이를 실증적으로 규명함으로써 국가차원에서 창업기업이 스케일업 할 수 있는 방안을 제시하는데 목적이 있다. 본 연구는 글로벌기업가정신모니터(GEM)의 일반성인조사 3.5년 미만의 초기 기업가들을 대상으로 하였으며, 국가경제발전단계를 혁신주도형, 효율주도형, 요소주도형 경제로 구분하여 R 3.5.0프로그램을 사용하여 국가경제발전단계 간 비교를 위해 다층모형분석을 통해 연구가설을 검증하였다. 가설검증 결과는 다음과 같다. 창업기업의 혁신지향성과 성장 열망의 영향관계에 있어 국가경제발전 간, 기업가 간 차이가 있는 것으로 나타났다. 국가의 경제가 발전할수록 기업가의 혁신활동이 더 두드러지게 나타난다. 또한 창업기업은 기업가의 영향을 많이 받기 때문에, 동일한 환경 내에서 기업가가 얼마나 혁신 지향적인가에 따라 열망의 정도에 차이가 있다고 할 수 있다. 창업기업의 혁신지향성과 성장 열망의 영향관계에 있어 실패에 대한 두려움은 국가경제발전 간, 기업가 간 차이가 있는 것으로 나타났다. 기업가 및 창업에 대한 실패에 대한 두려움은 국가경제발전 단계별로 차이가 있으며, 이러한 국가적 측면에서 실패에 대한 인식은 창업활동에 영향을 미치는 중요한 요인 중 하나이다. 이러한 연구결과를 통해 규명된 창업기업이 스케일업 기업으로 성장하는데 있어 성장열망에 영향을 미치는 검증된 요인을 국가경제발전단계에 따라 적합한 스케일업 생태계를 조성하는데 활용할 수 있을 것으로 기대한다.

• Asian Pacific Journal of Cancer Prevention
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• 제15권22호
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• pp.9679-9685
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• 2014

Background: When evaluating health-economics for cervical cancer prevention policies in Japan, it is important to use Japanese value settings. This study aimed to obtain preference-based measures (preference measures) for hypothesized health states among healthy Japanese women, and to examine differences between the EuroQol-5D (EQ-5D) and standard gamble (SG) instruments. Materials and Methods: The investigation was performed among female students at a nursing university. We used written hypothetical scenarios describing three grades of cervical intraepithelial neoplasia (CIN) and eight stages of cervical cancer, both at diagnosis and after medical intervention. Preference measures were evaluated using both EQ-5D and SG. Results: We received responses from 136 women. The mean number of respondents per stage was 24.6 (SD: 2.7). At diagnosis, average EQ-5D scores for CIN1, CIN2, CIN3, IA1, IA2, IB1, IB2, IIA, IIB, III, and IV stages were 0.84 (0.14), 0.78 (0.12), 0.73 (0.10), 0.78 (0.12), 0.72 (0.12), 0.63 (0.13), 0.64 (0.12), 0.68 (0.08), 0.62 (0.13), 0.55 (0.21), and 0.18 (0.24), respectively. Using one-way analysis of variance with the Tukey-Kramer method for multiple comparisons (each stage vs. CIN1), we found significant differences for IB1 and more advanced stages (p<0.05). After medical intervention, corresponding EQ-5D scores were 0.84 (0.12), 0.81 (0.12), 0.84 (0.12), 0.80 (0.15), 0.78 (0.11), 0.64 (0.15), 0.63 (0.15), 0.71 (0.15), 0.50 (0.17), 0.52 (0.17), 0.21 (0.28). The multiple comparisons identified significant differences for IB1 and more advanced stages, excepting IIA (p<0.05). SG evaluations were more variable and relatively higher than EQ-5D evaluations. Conclusions: We obtained preference measures for three grades of CIN1-3 and eight stages of cervical cancer. In combination with appropriate sensitivity analyses, these preference measures will provide a basis for an economic evaluation of cervical cancer prevention in Japan. We suggest that EQ-5D is appropriate for cost-utility analysis of this topic.

• 자원환경지질
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• 제19권2호
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• pp.85-96
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• 1986

The Bupyeong Silver mine which is located approximately 35km west of Seoul is currently the leading silver producer in Korea. The deposits occur as stockwork deposits hosted in Jurassic pyroclastic rocks. Occurrences of ore deposits and mineral paragenesis suggest a division of mineralization into four stages: Stage I, deposition of iron oxide and base metal sulfides; Stage II, deposition of tin oxide and silverm inerals; stage III, deposition of native silver and other silver minerals; Stage IV, formation of pyrite bearing siderite veinlets, Silver minerals in ore are native silver, argentite, freibergite, pyrargyrite, canfieldite, polybasite, dyscrasite and Ag-Fe-S mineral. The most important silver mineral is native silver among them. Chemical composition of important silver minerals were determined by electron probe microanalyser. Assay, size and modal analyses for floatation products were carried out. In floatation products, relative proportion of native silver for total important silver minerals have following ranges: feed, 64.7 to 74.74 wt.%; A-cleaner concentrate, 80.58 to 98.79 wt.%; and final tailing, 28.12 to 72. 57 wt. %. Average degree of liberation for native silver in feed and A-cleaner concentrate are 60.49% and 77.57% respectively. Negative relationship can be recognized between native silver and argentite in their abundance and behavior in floatation precesses.

• 자원환경지질
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• 제33권1호
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• pp.19-30
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• 2000

The Sannae-Eonyang granitic rocks are a large fossil hydrothermal system containing the Sannae Mo-W fissure-vein type and the Eonyang amethyst deposits in the southeastern Kyongsang Basin. They evolved through similar stages showing the similarities in chemical and mineralogical compositions, fractionation trends and early magmatic fluids. Major, trace and rare earth element(REE) variations can be accounted for fractional crystallization combined with variable degrees of metasomatism. Based on the aqueous fluids exsolved directly from the crystallizing melt, the Sannae-Eonyang granitic rocks were emplaced at similar depth or pressure conditions. High temperature fluid interaction with the granitic rocks affects the elements such as K, Na, Rb, Ba, Sr, Eu, and heavy REE (HREE) mostly through feldspar re-equilibration. Although hydrothermal fluids produced partly positive Eu anomalies and HREE depletion in the granitic rocks at the Sannae Mo-W mine, the chemical concentrations defining fractionnation trends have survived the effects of alteration. Aqueous fluids exsolved from the crystallizing melt appears to be widespread, whereas fluids of moderate to low salinity and low-density with relatively high homogenization temperatures and $Co_2$-rich fluids appear to be mainly restricted and responsible for Mo-W and amethyst mineralization, respectively. Hydrothermal system of the Sannae-Eonyang granitic rocks represents repeated fluid events; from exsolution of aqueous fluids from the crystallizing melt, through fluid immiscibility and meteoric convection to later mineralization.

• 자원환경지질
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• 제17권4호
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• pp.245-258
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• 1984

Geoje copper ore deposits are fissure filled copper veins which developed in late Cretaceous pyroclastics, andesite and shale. Mineral paragenesis reveals a division of the hydrothermal mineralization into three stages: Stage I, deposition of pyrite, magnetite, specularite, quartz and chlorite; Stage II, deposition of chalcopyrite, sphalerite, galena, tetrahedrite, aikinite, cosalite, electrum, quartz and chlorite; Stage III, deposition of barren calcite. Filling temperatures of fluid inclusions in quartz of stage I range from 171 to $282^{\circ}C$ whereas fluid inclusions in quartz and sphalerite of stage II range from 213 to $262^{\circ}C$ and from 186 to $301^{\circ}C$ respectively. Salinities of fluid inclusions in quartz of stage I range from 5.2 to 11.2 weight percent equivalent to NaCl. Salinities of fluid inclusions in quartz and sphalerite of stage II range from 6.6 to 10.9 and from 7.1 to 14.4 weight percent equivalent NaCl. Salinities of ore fluid during major mineralization stage in this deposits reveal nearly the same ranges as those of many copper deposits in Koseong copper mining district which located about 30km apart from Geoje mine. But filling temperatures of fluid inclusions formed during major copper mineralization stage in this deposits show slightly lower than those of copper deposits in Koseong copper mining district.

• 자원환경지질
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• 제23권1호
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• pp.1-9
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• 1990

A couple of Au-Ag-bearing epithermal quartz veins of Cretaceous(87.9Ma) in age are developed in the Cretaceous(112Ma) granodiorite batholith which was emplaced in Mesozoic Baegyari sedimentary formation. Au minerals consist mostly of electrum with a 54.2-61.9 wt% Au and are closely associated with sulfide minerals including pyrite, chalcopyrite, pyrrhotite, galena and sphalerite. Homogenization temperatures of fluid inclusions in quartz, fluorite and calcite are $196-368^{\circ}C$ (avg. $240^{\circ}C$), $74-176^{\circ}C$ (avg. $115^{\circ}C$) and $75-200^{\circ}C$ (avg. $119^{\circ}C$) respectively. Sulfur isotopic compositions( +5- +8‰) of ore sulfides indicate a deep-seated sulfur origin. Oxygen isotope compositions of different stages of quartz vary from +5.6 to +9.3‰ and calculated ${\delta}^{18}O$ values of ore fluid at $250^{\circ}C$ range from -3.2 to +0.4‰, reflecting an isotopically evolved ore fluid mixed with a $^{18}O$ depleted meteoric water under the variable mixing ratios between hydrothermal and meteoric waters. Isotopic data of calcite minerals support the above conclusions.

• 자원환경지질
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• 제29권2호
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• pp.119-127
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• 1996

Electrum-sulfide minerals of the Namsan Au-Ag mine were deposited in two stages of quartz and calcite veins that fill fault planes in Mesozoic granitic rocks (230~155 Ma). The K/Ar radiometric dating of hydrothermal sericite indicates that mineralization is early Cretaceous age ($127{\pm}3.0Ma$). Mineralogic, fluid inclusion and sulfur isotopic data show that ore minerals were deposited at temperatures between $340^{\circ}C$ and $200^{\circ}C$ from fluid with salinities of 3 to 6 equiv. wt % NaCl. Evidence of fluid boiling (and $CO_2$ effervescence) indicates a maximum pressures of 100 bars. The formation temperature and $fs_2$, of Au-mineralization from the Namsan mines are mainly $280{\sim}230^{\circ}C$ and $10^{-11}{\sim}10^{-13}$ atm, respectively. Au deposition was likely a result of boiling caused to chemical change (pH, $f_{O2}$, ${\Sigma}_{H_2S{\cdot}{\cdot}}$) of ore-fluids. Sulfur isotope composition of sulfide minerals (${\delta}^{34}S=5.1$ to 8.2‰) are consistent with ${\delta}^{34}S_{{\Sigma}{H2S}}$ value of +6 to +7‰, suggesting an igneous source of sulfur partially mixed with wall-rock sulfur.

• The Journal of Asian Finance, Economics and Business
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• 제7권3호
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• pp.253-263
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• 2020

This study aims to analyze of existing concepts of female entrepreneurship, evaluation of women's entrepreneurship in Kazakhstan and development of recommendations for its development in the country. This paper begins by reviewing research on female entrepreneurship. In this research, authors proposed the methodological tools based on systematic approach using economic and statistic methods and 5Ms concept. Analysis algorithm consists of four stages: evaluation of women entrepreneurship scale and business directions, analysis of employment in women's enterprises and business environment in Kazakhstan. The main limitation of this study was the lack of some gender-related indicators on the development of entrepreneurship. Further, the obtained results showed strong and weak points of female entrepreneurship in Kazakhstan. According to the results, there has observed increase in contribution of women in social-economic development of the republic, women's entrepreneurial activity is increasing, and the number of enterprises headed by them is growing. However, the growth of female entrepreneurship occurs while maintaining their insignificance in terms of turnover and number of employees. There is a pronounced industry specificity of female entrepreneurship: the service sector. In accordance with this, there were identified priority areas and there were developed recommendations for the development of female entrepreneurship in Kazakhstan.