• CRM연구
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• v.3 no.2
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• pp.1-20
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• 2010

Due to the nature of teenage students' common tendency of being drawn to consumption conformity engendered by popular trends, and further expanding their unique collectivist culture, this study presumes that middle and high school female students as well have an influential factor that creates their distinctive trait. This study is intended to investigate the students' personal characteristics and effects of social reference groups, and further scrutinize how these influences transcends to deviant make-up behaviors. A total of 297 subjects, middle and high school female students, participated in a survey, using questionnaires focused primarily on the degrees of color makeup and the influences imposed by classmates. The findings of the study are as follows. First, regarding makeup behavior displayed by middle and high school female students, social self-esteem had positive influence on innovation and peer pressure. Second, perceived visibility conversely had negative impacts on innovation and peer pressure. This indicates that if perceived visibility is at a salient level, this already signifies lack of innovation. Third, makeup innovation and peer pressure demonstrated by middle and high school students all showed positive influence on their makeup behaviors. Additionally, peer pressure, in comparison to innovation, had greater influence on makeup behaviors, which indicates that peer pressure play a great role in makeup behavior of middle and high school students. Fourth, makeup behaviors showed strong impacts on makeup satisfaction and rendering deviant behaviors, which indicates that a new direction and perspective regarding middle and high school students' makeup behavior is critical.

• Korean Journal of Mineralogy and Petrology
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• v.35 no.4
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• pp.397-407
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• 2022

Mineralogical analysis of the bedrock of the Gobi Desert in southern Mongolia, the source of Asian dust, was conducted to trace the geological origin of the constituent minerals of Asian dust. The bedrock of the source of Asian dust consists of Paleozoic volcanics and volcaniclastic sedimentary rocks, Paleozoic granitic rocks, and Mesozoic sedimentary rocks. Paleozoic volcanics and volcaniclastic sediments lithified compactly, underwent greenschist metamorphism, and deformed to form mountain ranges. Mesozoic sedimentary rocks fill the basin between the mountain ranges of Paleozoic strata. In comparison to Paleozoic volcanic and sedimentary rocks, Mesozoic sedimentary rocks have lower contents of chlorite and plagioclase, but high contents of clay minerals including interstratified illite-smectite, smectite, and kaolinite. Paleozoic granites characteristically contain amphibole and biotite. Compared with the mineral composition of bedrock in source, Asian dust is a mixture of detrital particles originating from Paleozoic and Mesozoic bedrocks. However, the mineral composition of Mesozoic sedimentary rocks is closer to that of Asian dust. Less lithified Mesozoic sedimentary rocks easily disintegrated to form silty soils which are deflated to form Asian dust.

• 건강소식
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• v.34 no.9
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• pp.26-27
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• 2010

결혼 후 불임으로 인해서 마음고생이 이만저만이 아닌 부부들이 늘고 있는 추세이다. 불임의 원인으로는 과도한 흡연, 음주, 무정자증, 배란장애, 조기폐경, 각종질환, 환경적인 요인 등 다양하며, 비만도 불임의 한 원인이 된다. 외국의 한 통계자료에 의하면 불임 환자의 6%는 비만이 원인인 것으로 나타났다. 혹시 불임으로 고생하고 있다면 비만이 원인은 아닌지 진단해 보자.

• The Journal of the Petrological Society of Korea
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• v.5 no.2
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• pp.168-187
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• 1996

In the study area Uanggunbong-Samgunri area), Precambrian metamorphic complex, (Taebacksan gneiss complex, Hyundong gneiss complex, and Taebacksan schist complex) had undergone three different regional metamorphisms at least before Paleozoic. The Paleozoic sediments in the study area also had undergone three different metamorphisms at least. The first is low pressure type regional metamorphism, the second is low pressure type contact metamorphism due to the intrusion of Chunyang granite, and the last is medium pressure type metamorphism caused by thrust in south of Janggunbong area. The first metamorphism formed the prevailing metamorphic zones in the Paleozoic metasediments and the metamorphic grade of the first regional metamorphism increases from the chloritoid zone, through the staurolite zone, garnet zone, staurolite+biotite zone, and to the andalusite+biotite zone. The second metamorphism affected both Pre-Cambrian and Paleozoic metasediments located close to the Chunyang granite. The effect of the contact metamorphism is restricted to the very narrow zone around the granite. The third metamorphism that produced kyanite, is restricted to the very narrow region near the thrust fault in the south of Janggunbong with an E-W trend.

• Journal of the Korea Academia-Industrial cooperation Society
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• v.22 no.1
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• pp.691-702
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• 2021

This study aimed to provide basic data for safety education by surveying the status of safety education and general safety awareness among high school students by gender and school type in Chungnam area. From July 16th to October 15th, 2015, 1214 copies collected from 16 schools were analyzed using SPSS ver 23.0. Regarding safety education, females and general high school students (GHS) responded more frequently that safety education was more necessary for school life compared to males and specialized high school students (SHS), whereas males were more interested in safety education content than females. Males and SHS lost interest when learning unfamiliar content compared to females and GHS, respectively. In terms of general safety awareness, males and GHS usually followed safety rules better than females and SHS, and males demonstrated greater knowledge of first aid. Males and SHS acted according to their beliefs towards safety rather than knowledge compared to females and GHS, respectively. This study found a significant difference in safety education and general safety awareness among high school students by gender and type of school, and the results suggest that differentiated safety education is necessary.

• Journal of the Speleological Society of Korea
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• v.40
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• pp.10-12
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• 1994

중국에 있는 대형동굴로서는 주로 용식동굴이다. 용식동굴의 지리적 분포는 지질상황과 기후조건에 의하여 결정된다. 지질상황은 용식동굴이 이루어 질수 있는 토대이고 기후상황은 용식동굴이 형성될 수 있는 동력적 인소이며 지질구조는 용식동굴이 형성될수 있는 조건이다. 중국 지질사에서 보면 원생대로부터 고생대 중생대에 이르면서 여러차례의 해침, 해퇴가 있었는데 그중에서도 고생대의 해침에 의하여 형성된 석희암이 많다. 중생대에도 해침현상은 있었으나 이때의 퇴적상중에는 석회암상이 매우 적었다. 원생대 시기의 퇴적상중에는 석회암이 적지 않으나 그후의 침식작용을 받아 암층이 엷어졌고 또 내려작용을 받아 변성되어 대리암으로 되었거나 상승된데서 지하수위가 떨어져 용식동형성이 불가능하다. 때문에 중국에 있는 대형동굴은 일반적으로 고생대의 석회암층에 많이 분포되었다.(중략)

• Cement
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• s.12
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• pp.47-52
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• 1965

• Economic and Environmental Geology
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• v.49 no.2
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• pp.155-165
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• 2016

Quartz schist - quartzite is often intercalated in metasedimentary rocks of Ogcheon belt or aligned parallel to the boundary between Yeongnam massif and Ogcheon belt. However, stratigraphic sequence and or geologic age of the rocks has been still variable among authors as Precambrian or Paleozoic. In this study, we carried out SHRIMP U-Pb age data of detrital zircons from Yeongam and Yeongsanpo areas and compared ours with other zircon ages from other areas. The detrital zircons from the studied area show no age younger than 1.8 Ga but yielded clusters at Neoarchean (2.5 Ga) and Paleoproterozoic (1.8 Ga). On the other hand, the age range of zircon U-Pb dating of Paleozoic quartzites yielded from Archean to middle Paleozoic and clusters at Paleoproterozoic, Neoproterozoic and Paleozoic. The characteristics of the zircon age range and the dominant age peak might become a key to classify the Proterozoic to Paleozoic quartz schists-quartzites, which ages are still remained under controversy. Based on the statistical results of the zircon ages in this study, quartz schist - quartzite from Yeongam and Yeongsanpo is considered to be deposited during Proterozoic.

• 한국디지털정책학회:학술대회논문집
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• 2006.12a
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• pp.421-431
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• 2006

지식정보사회의 핵심 키워드인 e-learning은 많은 발전을 하고 있다. e-learning은 오프라인 교육에 비해 시간과 공간의 제약을 받지 아니하고, 비용이 저렴하며 반복 학습과 개인화된 서비스가 가능하다는 장점이 있는 반면에 아직도 파급 효과는 크지 못한 실정이다. 또한 국가적인 차원에서 많은 지원을 하고 있고 시장의 급속한 성장과 확산에 비해, 중${\cdot}$고생들을 대상으로 하는 e-learning사이트의 컨텐츠 품질에 대한 연구는 미비한 실정이다. 이에 본 연구에서는 중${\cdot}$고생 시절에e-learning의 경험이 있는 대학생들을 중심으로 실증연구를 수행하였다.

• The Korean Journal of Quaternary Research
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• v.8 no.1
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• pp.23-32
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• 1994

고생대(폐름기)의 육성 퇴적층(옥갑산층) 일부분이 고기 우각호(ox-bow lake)에 서 퇴적된 것으로 해석된다, 옥갑산층의 하부층서의 일부분은 암회색 이암/담회색 사암의 호층 단위가 평균 5.1cm 두께로 약 80회반복하는 암상을 나타낸다. 이 암상의 퇴적환경은 층서적 상하 암상의 연합에 근거하면 해안 평야로서 하천 범람원 분지의 쇄설성 퇴적환경의 일부이 면서 사행천과 연관된 우각호 퇴적환경으로 해석된다.