• KDI북한경제리뷰
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• v.21 no.9
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• pp.41-59
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• 2019

• KDI북한경제리뷰
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• v.23 no.3
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• pp.37-45
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• 2021

• Analyses & Alternatives
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• v.8 no.3
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• pp.7-44
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• 2024

This article attempts to analyze the changes and prospects of the Northeast Asian security environment in the era of New-Cold War & multipolarity that has been spreading since the outbreak of the US-China strategic competition and the war in Ukraine. Since the war in Ukraine, changes in the new strategic triangle between the United States, China, and Russia have begun to have an unprecedented impact on the Northeast Asian security environment. This article analyzes how the two factors, the U.S.-China strategic competition and the war in Ukraine, have led to changes in the Northeast Asian security environment. More specifically, the recent changes and prospects of the China-Russia-North Korea triangle and the three bilateral relationships, China-Russia, China-North Korea, and Russia-North Korea. To analyze this research topic, the research design is based on three variables: independent, mediating, and dependent variables. The independent variables are changes in U.S.-China relations and changes in U.S.-Russia relations. The mediating variables are the US-China strategic competition and the war in Ukraine. On the one hand, the confrontation between the U.S.-China relationship led to a strategic competition, and on the other hand, the conflict between the U.S.-Russia relationship led to the war in Ukraine. In addition, the two independent variables can only be influenced by the two mediating variables. In particular, we assume that the domestic political factors of the three major powers, the United States, China, and Russia, played a significant role in causing the two mediating variables. The independent variables and mediating variables work together to promote the Northeast Asian security crisis. As a result, threats to the Northeast Asian security environment have emerged as the dependent variable. The dependent variables are the North Korea-China-Russia triangle, changes in the three bilateral relationships within the triangle, and the confrontation of Northern Triangle versus Southern Triangle. The first mediating variable, strategic competition, has led to several changes in the Northeast Asian security environment: the quasi-alliance of Sino-Russian relations, the restoration and strengthening of North Korea-China relations, the strengthening of trilateral security cooperation between the United States, Japan and South Korea, and the increasing necessity of Sino-Russian-North Korean trilateral cooperation. The second mediating variable, the war in Ukraine, has led to the strengthening of Sino-Russian relations, re-alignment of North Korea-Russia relations, the promotion of the US-Japan-ROK triangular alliance, and the emergence of the China-Russia-North Korea triangular cooperation.

• Journal of the Economic Geographical Society of Korea
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• v.20 no.3
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• pp.267-286
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• 2017

The main purpose of this paper is to identify the spatiality of North Korea and China border regions through investigating the exceptional characteristics of the regions with the concept of positionality, which allows us to realize the relative position between subject and object. Border regions could be identified appropriately by considering the concept of switching positionality, as it is a kind of multiple space in which its sudden closure and opening should be configured in accordance with geopolitical and geoeconomic changes centering around border line. The main arguments of this research concerned with border regions with the concept of switching positionality are fallen into three. Firstly, changes in border regions should be analyzed by investigating more broader contexts and conjunctural perspectives, and even an internal condition stemmed from locality. Secondly, trajectories of border regions could be analyzed by the assemblages of various powers. Finally, the positionality of economic actors should be examined by identifying dynamic relations between geoeconomics and geopolitics. In particular, the concept of positionality has led to a number of insights into discussions on time-space, and spatiality in relational-dialectical, socio-spatial, and power-topological perspectives. Based upon this concept of positionality, the research has identified exceptional characteristics in North Korea and China border regions. It argues that the exceptionality of the region has stemmed from the intersection between the unstability of geopolitical security and various geoeconomic benefits.

• Journal of the Korean earth science society
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• v.36 no.7
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• pp.643-648
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• 2015

Equations that could estimate the local magnitude of historical earthquakes, being difficult to calculate, in Sino-Korea craton was obtained using instrumental earthquake data for 22 Korean and 46 northeastern Chinese events. The obtained equations from intensity $I_0$ is $M_L=1.7+0.57{\times}I_0$. The equation from felt area FA for the Korean Peninsula is $M_L=4.29-1.34{\times}log(FA)+0.28{\times}log^2(FA)$. When the information on earthquake damage, effects, and felt area is all recorded at the same time, the former equation of intensity is more feasible than that of felt area due to uncertainty in earthquake felt area.

• 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.

• Journal of the Economic Geographical Society of Korea
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• v.20 no.3
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• pp.369-387
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• 2017

This research derived sum of light (SOL) for Liaoning and Dandong, China, from DMSP OLS satellite images acquired at nighttime during 1992 to 2012 and investigated its potential association with economic status. The SOLs of Liaoning were found to be continuously increasing and higher than those of averages for the other provinces across the time period. The temporal pattern of SOLs would be interpreted to well reflect the economic status of this region based on real growth rate and average wage per capita. Nevertheless, the SOLs of Dandong were lower than the average of the other prefecture-level cities, which indicated the economic status of this city in China. Meanwhile, the average annual growth rate of SOLs for Dandong turned out to be increase for 1998~2007, compared with the previous years, and temporal patterns in the trade amount between North Korea and China and the export amount of North Korea to China were similar to those of SOLs in the same time period. The political association between South and North Koreas was improved with 'Sunshine Policy' during 1997~2007. Taking it into account, SOL is expected to be valuable spatial proxy index that could explain the geopolitcal and geoeconomic aspects of Dandong.

• The Journal of the Petrological Society of Korea
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• v.21 no.2
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• pp.129-150
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• 2012

The tectonic evolution of the Central Ogcheon Belt has been newly analyzed in this paper from the detailed geological maps by lithofacies classification, the development processes of geological structures, microstructures, and the time-relationship between deformation and metamorphism in the Ogcheon, Cheongsan, Mungyeong Buunnyeong, Busan areas, Korea and the fossil and radiometric age data of the Ogcheon Supergroup(OSG). The 1st tectonic phase($D^*$) is marked by the rifting of the original Gyeonggi Massif into North Gyeonggi Massif(present Gyeonggi Massif) and South Gyeonggi Massif (Bakdallyeong and Busan gneiss complexes). The Joseon Supergroup(JSG) and the lower unit(quartzose psammitic, pelitic, calcareous and basic rocks) of OSG were deposited in the Ogcheon rift basin during Early Paleozoic time, and the Pyeongan Supergroup(PSG) and its upper unit(conglomerate and pelitic rocks and acidic rocks) appeared in Late Paleozoic time. The 2nd tectonic phase(Ogcheon-Cheongsan phase/Songnim orogeny: D1), which occurred during Late Permian-Middle Triassic age, is characterized by the closing of Ogcheon rift basin(= the coupling of the North and South Gyeonggi Massifs) in the earlier phase(Ogcheon subphase: D1a), and by the coupling of South China block(Gyeonggi Massif and Ogcheon Zone) and North China block(Yeongnam Massif and Taebaksan Zone) in the later phase(Cheongsan subphase: D1b). At the earlier stage of D1a occurred the M1 medium-pressure type metamorphism of OSG related to the growth of coarse biotites, garnets, staurolites. At its later stage, the medium-pressure type metamorphic rocks were exhumed as some nappes with SE-vergence, and the giant-scale sheath fold, regional foliation, stretching lineation were formed in the OSG. At the D1b subphase which occurs under (N)NE-(S)SW compression, the thrusts with NNE- or/and SSW-vergence were formed in the front and rear parts of couple, and the NNE-trending Cheongsan shear zone of dextral strike-slip and the NNE-trending upright folds of the JSG and PSG were also formed in its flank part, and Daedong basin was built in Korean Peninsula. After that, Daedong Group(DG) of the Late Triassic-Early Jurassic was deposited. The 3rd tectonic phase(Honam phase/Daebo orogeny: D2) occurred by the transpression tectonics of NNE-trending Honam dextral strike-slip shearing in Early~Late Jurassic time, and formed the asymmetric crenulated fold in the OSG and the NNE-trending recumbent folds in the JSG and PSG and the thrust faults with ESE-vergence in which pre-Late Triassic Supergroups override DG. The M2 contact metamorphism of andalusite-sillimanite type by the intrusion of Daebo granitoids occurred at the D2 intertectonic phase of Middle Jurassic age. The 4th tectonic phase(Cheongmari phase: D3) occurred under the N-S compression at Early Cretaceous time, and formed the pull-apart Cretaceous sedimentary basins accompanying the NNE-trending sinistral strike-slip shearing. The M3 retrograde metamorphism of OSG associated with the crystallization of chlorite porphyroblasts mainly occurred after the D2. After the D3, the sinistral displacement(Geumgang phase: D4) occurred along the Geumgang fault accompanied with the giant-scale Geumgang drag fold with its parasitic kink folds in the Ogcheon area. These folds are intruded by acidic dykes of Late Cretaceous age.