• Land and Housing Review
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• v.6 no.2
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• pp.79-88
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• 2015

North Korean leader Kim, Jung-Il visited Beijing, China, May 2010, when he made a common recognition with Chinese President Hu Jintao on construction of the Rasun SEZ and the Hwanggumpyong-Wyhwado SEZ for development of Economic cooperation between N.Korea and China and accelerating establishment of SEZs in N.Korea. However, after N.Korea's third nuclear test on Feb. 2013, the relationship between N.Korea and China became a little worse. Recently, three nations' border region near Rasun in N.Korea is reconsidered that it is very important place for collaboration between and among 2, 3 or 4 countries, S.Korea, N.Korea, China and Russia. This thesis examined these changes of cooperation and plans among the countries near the border region and proposed some measures for participation of S.Korea on the projects in the Rasun region.

• NEWSLETTER 전기공업
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• no.94-20 s.117
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• pp.17-40
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• 1994

• NEWSLETTER 전기공업
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• no.94-7 s.104
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• pp.18-40
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• 1994

• Journal of the Korean association of regional geographers
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• v.15 no.5
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• pp.590-603
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• 2009

This report studies what connections was between Ethnic education movement in Bukkando and natural and human knowledge environment as a way to complement total absence of studying Anti-Japanese Movement at the Geographic levels. The summary is as following: At first, the Korean villages, where almost all spread the national schools, so there was a very close relationship. Both from a Longjing as the central plain area to the proliferation of surrounding areas. Second, schools that was adjacent to trunk road were given a great deal of weight on the connection with traffic. After that, however, it decreased gradually. Third, the national schools suffered the dual intervention from China and Japan, experienced a difficult development process. the schools which built by Japan were spreaded areas where concentrate the schools which built by Japan were spreaded areas where concentrated many national schools, both have a close relationship. before 3.13 movement, the distribution of schools that established by the Chinese mainly spreaded the areas concentrated national schools. But, after the 3.13 movement, it appeared a tendency to spread to the Korean people area where relatively dwelled a few people.

• The Korean Journal of Quaternary Research
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• v.2 no.1
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• pp.51-85
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• 1988

The understanding of the faunal sequence and palaeoenvironment of East Asia since the Late Tertiary depends mainly on the knowledge of Chinese fauna and its environmental changes. The recent Chinese researches including geology, geomorphology, climats fluctuation and loess distribution of this area have provided that the rapid uplifting of Himalayas and Qinghai/Xizang Plateau since the Lower Pleistocene was a main selective factor for the process of environmental changes in this vast territory. Although different concepts of the Plio-Pleistocene boundary have been provided, its boundary can not exceed over 2 mya. Instead of the traditional zoogeographical dicthomy in China, faunal compositions of Pleistocene are divided into three faunal zones. The knowledge of macrofaunal evolution in China are useful to understand the palaeoecology of East Asia. Palaeoenvironment of Korea during the Pleistocene Period can be reconstructed by using the analogy of the current Chinese studies.

• Economic and Environmental Geology
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• v.52 no.3
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• pp.213-221
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• 2019

The Wugang banded iron formation (BIF) is located within the Taihua complex at the southern margin of the North China Craton (NCC). In this study, we analyzed major elements and rare-earth elements in iron ores from the Wugang BIF, to study the type of BIFs and their formation mechanism in combination with previously-published data from the literature. We found that the iron ores from the Wugang BIF display two types of banding textures, which can be described as weak banding or no banding. The samples are composed of coarse-grained magnetite, quartz, pyroxene, and amphibole. Based on our geochemical results, mixing of a hydrothermal fluid with sea water led to the precipitation of the Wugang BIF, and there is evidence of crustal contamination. These results, combined with previous literature data, almost all of the iron ores lack Ce anomalies, though some samples show negative Ce anomalies. Our results indicate that the Wugang BIF was formed in a dominantly reducing environment, although the surfaces were relatively oxidized. Geochemical evidence suggests that the Wugang BIF iron ores were formed in a near-shore continental-shelf environment or in a back-arc basin. The BIF is known as interbedded with migmatite, amphibole gneiss, minor quartz and marble, which indicating lack of volcanic materials input. This study, combined with previous results on geochemical interpretation of related wall rock of Wugang BIF, demonstrated that Wugang BIF belongs to Superior-type BIF.

• 한국방재학회:학술대회논문집
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• 2010.02a
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• pp.113.1-113.1
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• 2010

본 연구에서는 1951~2008년까지 58년 동안 북한에 상륙한 태풍의 빈도, 강도, 진로 및 피해 특성에 대해 분석하였다. 분석 기간 동안 태풍 빈도는 감소하고 강도는 약해지는 추세였다. 이러한 강도 변화는 대부분의 태풍이 온대저기압 상태로 약화된 후에 북한에 상륙하여 영향을 주었기 때문이다. 태풍 진로는 중국과 남한을 경유하거나 서해안에 직접 상륙하는 3가지 유형으로 분류되었다. 북태평양고기압과 태풍 진로와의 관련성 분석에서 북태평양고기압은 태풍이 중국을 경유하여 상륙할 경우 서쪽으로 확장하였고, 서해안에서 직접 상륙할 경우와 남한을 경유하여 상륙할 경우에는 북쪽으로 확장 발달하였다. 또한, 태풍 재해가 발생한 총 5건의 사례 중에서 2000년 프라피룬은 서해안에 직접 상륙하였으며 바람에 의하여 약 60억 달러의 경제적 피해가 발생하였고, 2002년 루사는 남한을 경유한 후 상륙하였으며 강수에 의해 약 50만 달러의 경제적인 피해가 발생하였다.

• The Journal of the Petrological Society of Korea
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• v.18 no.2
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• pp.171-179
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• 2009

LA-ICP-MS U-Pb zircon age was determined from the granite gneiss from Jeungsan-Pyeongwon area located to the west of Pyeongan Basin, North Korea, yielding concordant age of $1,873{\pm}19(2{\sigma})$Ma interpreted as Paleoproterozoic granitic magmatism. Considering relatively precise data reported recently using SHRIMP and LA-ICP-MS, ages around 1,870 Ma have been most frequently reported from Precambrian basement rocks of Korean peninsula, including Yeongnam, Gyeonggi, and Nangnim massifs altogether. Geologic events of this period are interpreted as not only granitic magmatism but also hightemperature regional metamorphism depending on their localities. The magmatic and regional metamorphic events of similar periods have also been reported from neighboring cratons of both North China and South China. Therefore, we need more data and efforts to decipher correlation between Precambrian basements between Korea and China.

• Journal of Digital Convergence
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• v.15 no.11
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• pp.187-197
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• 2017

The purpose of this study is to analyze factors that have significant influence on decision making of inland transportation of shippers. The study was conducted in Republic of Korea and Northern areas of China where marine feeder lines are operated, and logistic regression analysis was used as a research method. More than 67% of the domestic shippers who received the questionnaire were found to make inland transportation decisions. As a result, the inland freight and unloading costs had a significant influence on the inland transportation decision of the shippers. On the other hand, in order to attract domestic and overseas shippers to generate profits, it is necessary to establish various infrastructures and incentives for government support to reduce inland transportation costs and freight charges by identifying needs of shippers. In addition, it is necessary to review the factors influencing decision making of inland freight in shippers and port facilities, and ways to create freight should be sought through continuous improvement efforts in these areas. An analysis using various factors which can influence inland transport is needed as a future study.

• The Journal of the Petrological Society of Korea
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• v.19 no.3
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• pp.199-208
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• 2010

The Cenozoic alkali basalts are distributed over Korea, both on central part as Bangnyeongdo, Ganseong, Pyeongtaek-Asan and Jogongni and also on southernmost part Jejudo. The ultramafic mantle xenoliths carried by Korean alkali basalts are spinel lherzolites. Garnet lherzolite that is more stable at the deeper level has not been reported so far, indicating that the lithospheric thickness under Korea does not reach deep enough to the stable zone of garnet lherzolite. The crustal evolution history of the Korean peninsula, at least some part of it, seemingly started since the Archean, it normally should have lithospheric thickness greater than 150 km. However, the mantle xenoliths carried by the Cenozoic alkali basalts indicate the maximum depth of origination in the much shallower range of 60-90 km. Such significantly thinner lithospheric thickness of the Korean peninsula than expected is quite similar to the case of North China Craton having lithospheric thickness of ca. 80 km in average, suggesting thinning of the lithospheric mantle in a depth scale of a few tens of kilometers during the past geologic time. The main causal events for such significant thinning of the lithospheric mantle can be continental collisional events of Paleoproterozoic and early Mesozoic similar to the case of North China Craton, which are also supported by Paleoproterozoic igneous and metamorphic events during the 1.9-2.0 Ga occurring all over the Korean peninsula and also early Mesozoic continental collisional event which has been discussed on lively arguments.