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스토리 창작 교육에 있어 캐릭터 구축을 위한 실습 프로그램 개발 연구
김의준 한국예술교육학회 2023 예술교육연구 Vol.21 No.3
In story creation, characters, along with plots, have traditionally been emphasized in their importance. Therefore, the theory of character setting is dealt with as a major part in most writing books. Even in story creation education, learning about the theory that composes a character along with the plot and its practice occupy an important portion. In order to develop the character build- ing ability required for story creation, it is necessary to first learn the main theories required for character setting and practice each theory. However, there are no studies or explanations on the in- terrelationships of the separate personality theories acquired in the individually conducted educa- tional process, and there are not many cases of integrating them into practice programs and applying them to the educational process. The theories required for character building can be largely divided into two categories. These are the theories about the type of character and the theory about the character's journey (arc). The main theories that explain the type of character include the Enneagram, MBTI, and TIPI. Regarding the character's inner journey, there is the Character Arc Theory, which explains the change of the character with positive arc, negative arc, and flat arc. However, these major theories have a problem in that they are individually applied in a state where the interrelationship is not clearly identified. Even in the case of ‘LIE’, the main concept of character arc, it is inevitably influenced by the type of character, but due to the absence of a con- cept that comprehensively explains it, creators are experiencing various confusions in the actual cre- ation process. Individually applied theories like this can hinder the unity in character composition of characters, which can act as an obstacle for each character to express their personality. Therefore, this study revealed the theories necessary for character construction and the interrelationships be- tween the theories, focusing on the value concept of the controlling idea, and applied it to practice in the form of a personality table to develop an integrated practice program for character con- struction and check its effectiveness
지역 및 도시개발의 문제와 대책 : 도시정주체계와 도시경제문제 ( Urban Hierarchy and Its Economic Problems )
김의준 대한건축학회 1993 建築 Vol.37 No.7
우리나라의 도시정주체계의 변화는 정부의 비공간적 개발전략이 투영되는 과정이다. 특히 생산요소의 공간적인 집적을 통한 효율성의 추구는 일부 대도시 및 제조업 특화도시를 발전시켰으나, 결과적으로 대도시와 중소도시, 도시와 농촌 등의 서로 다른 공간개체간의 왜곡된 개발양식을 창출하였다. 물론 1960년대의 경공업 중심의 수출전략과 1970년대의 중화학 공업육성을 통한 수입대체 발전전략은 도시의 경제적 성숙도를 더하였으나. 일부 대도시의 급속한 성장은 도시기능을 올바르게 수행하지 못할 뿐만 아니라 지방중소도시의 성장잠재력을 제대로 활용하지 못하고 오히려 중소도시의 인력유출에 따른 경제성장기반을 위축시키게 되었다.
김의준,양석준,신승욱,남형태,신동복,임헌경,오일환,노상건,조성준,박맹언 한국지질과학협의회 2018 Geosciences Journal Vol.22 No.6
The Geodo skarn deposit is located in the Taebaeksan Basin, central eastern Korean Peninsula. The geology of the deposit consists of Cambrian to Ordovician calcareous sedimentary rocks and the Cretaceous Eopyeong granitoids. The skarns at Geodo occur around the Eopyeong granitoids, which consist, from early to late, of magnetite-bearing equigranular quartz monzodiorite, granodiorite, and dykes. These dykes emanated randomly from equigranular granodiorite and some of dykes spatially accompany skarns. Skarn Fe mineralization, referred as Prospect I and II in this study, is newly discovered beyond previously known skarns adjacent to the quartz monzodiorite. These discoveries show a vertical and lateral variation of skarn facies, grading from massive reddish-brown garnet-quartz in a lower and proximal zone to banded in an upper and distal zone, reflecting changes in lithofacies of the host rocks. Skarn veins in distal locations are parallel to sedimentary laminae, suggesting that lithologic control is important although proximal skarn has totally obliterated primary structures, due to intense retrograde alteration. Skarns at Geodo are systematically zoned relative to the causative dykes. Skarn zonation comprises proximal garnet, distal pyroxene, and vesuvianite (only in Prospect I) at the contact between skarn and marble. Retrograde alteration is intensely developed adjacent to the contact with dykes and occurs as modification of the pre-existing assemblages and progressive destruction such as brecciation of the prograde assemblages. The retrograde alteration assemblages consist predominantly of epidote, K-feldspar, amphibole, chlorite, and calcite. Most of the magnetite (the main ore mineral), replaces calc-silicate minerals such as garnet in the lower proximal exoskarn, whereas it occurs massive in distal pyroxene and amphibole in the upper and distal exoskarn. The emanation of dykes from the equigranular granodiorite has provided channelways for ascent of skarn-forming fluids from a deep source, whereas the style and nature of skarns suggest that originally structurally-controlled skarn-forming fluids may migrate long distances laterally to produce skarn in calcareous sedimentary rocks.