민진당 정부의 대만독립노선과 양안관계

김옥준 사단법인 한국평화연구학회 2009 평화학연구 Vol.10 No.1

The Democratic Progressive Party which had succeeded to get power by elaborating its Taiwan identity began to advocate Taiwan independence policy. However, the issue of Taiwan independence is not only related with complex international politics but it also would be almost impossible if China does not abandon the "One China Policy". Then, what kinds of implications can be generated by insistence of the Democratic Progressive Party's Government about Taiwan Independence on Cross-Straits Relations? And while the political tension between China and Taiwan has been intensified due to the Taiwan independence policy of DPP's government, why the relations between China and Taiwan have been constantly maintained in non-political issue-areas? In this regard, this paper firstly examines how DPP's government began to advocate Taiwan independence policy from the Taiwanese perspective. Second, it attempts to define why the political tension has not determined Cross-Straits Relations in non-political issue areas by investigating progresses of the interactions and cooperation among Taiwanese opposition party and civilian sectors with Chinese counterparts. Finally this paper identifies strengths and limits of Taiwan independence policy of DPP's government based on the results of the research. 대만인의 정당이라는 정체성을 가지고 정권교체에 성공한 민진당은 그들의 정치적 신념인 대만독립을 표방하게 된다. 그러나 대만독립이란 복잡한 국제적인 문제 일뿐만 아니라 중국이 ‘하나의 중국’원칙을 포기하지 않는 한 실현되기는 어렵다는 것은 모두가 주지하고 있는 사실이다. 그렇다면 민진당 정부의 대만독립주장은 양안관계에서 어떠한 의미를 가지고 있는가. 또한 민진당 정부의 대만독립의 주장으로 인한 정치적 관계의 긴장에도 불구하고 비정치적인 영역에서의 양안관계는 꾸준히 발전하고 있는 양안관계의 본질은 무엇인가. 본 논문은 이러한 의문에서 출발하여 주로 대만의 입장에서 민진당 정부의 대만독립노선이 실제로 어떻게 표출되었으며, 정치적 긴장이 고조되고 있었음에도 불구하고 야당과 민간 부문에서의 양안간의 교류와 협력이 어떻게 진전되고 있었나를 밝혀 봄으로써 정치적 긴장이 비정치적 영역으로 파급되지 않는 양안관계의 실태를 입증 한 후, 이를 바탕으로 민진당 정부의 ‘대만독립’노선의 성격과 한계점을 고찰 해보고자 한다.

치성 낭종에서 염증 반응이 Ki-67 _ Cox-2와 Glut-1 항체의 분포에 미치는 영향

김옥준,김한일,최홍란 대한구강악안면병리학회 2004 대한구강악안면병리학회지 Vol.28 No.2

Department of Oral Pathology, Dental Science Research Institute, College of Den디'suy, Chonnam National University It is well known that the expansion of radicular and dentigerous cyst is related to the change of osmotic pressure, while the prolifera디on ofthe 비피19 epithelium in odontogenic keratocyst. When the dentigerous cyst and odontogenic keratocyst has secondary infection, they present the loss of unique sπuctures and epithelial hyperplasia. There is a question whether inflammatory reaction affects cystic formation, expansion and their treatment. Present study is to evaluate the relationship between inflammation and epithelial hyperplasia using immunohistochemial study. Followings are result; 1. 까1e age of patients ranged from 10 to 73 years (mean age, 39 years) in radicular 이5t, 10 to 71 years (mean age, 35 years) in dentigerous cyst and 10 to 54 years (mean age, 23.4 years) in odontogenic keratocyst. The sex distribution of patient distributed 32 cases for male and 16 cases for female in radicular cyst, 13 and 10 in dentigerous cyst and equally 5 and 5 in odontogenic keratocyst. 2. Inflammatory cyst in the present study distributed 44/48 cases (9 1.7%) for radicular cyst, 15/ 23 cases for dentigerous cyst and 1/ 10 case for odontogenic keratocyst. 3. Evaluation of inflammatory reaction and antigen expression, ki-67 , cox-2 and glut-1 expression increase in the inflammatory radicular and dentigerous cyst. 4. In odontoge띠c keratocyst, expression of antigens increase regardless of inflammation. Above results showed that inflammation stimulate the proliferation of lining epithelium leading to cystic expansion.

함탄층(含炭層) 내의 chiastolite-shale의 개발(開發) 이용(利用)에 관(關)한 연구(硏究)

김옥준,김규한,Kim, Ok Joon,Kim, Kyu Han 대한자원환경지질학회 1975 자원환경지질 Vol.8 No.3

The chiastolite bearing shale was known to occur in various coal fields in South Korea among which the Kangneung coal fields is the most outstanding in quality and quantity of chiastolite. The chiastolite occurs mostly in black shales of Sadong formation and little in shales of Hongjom and Kobangsan formations, and is most abundant in the footwall coaly shales of the Sadong coal seams. The chiastolite has been proved to be thermal contact product of the high aluminous shale that comes into contact with Kangneung granite. The distribution of chiastolite in the Kangneung coal field is irregular. The eastern part of the region contains more chiastolite than that of western part. It is believed that the difference of the grade is due to the intensity of metamorphism. The grade of chiastolite in the shale varies from few percent up to as high as 60 % in volume, and the minable reserve of the chiastolite is estimated about 4,700,000 tons. This reserves is rather concentrated in few localities such as in Jiam Mine, Jungrim Mine, Sir 1 Hang in the Whasung Mine, the second and third sections of Kangneung Mine and Umbuelri district. The chemical composition of chiastolite bearing coaly shale is $SiO_2$, 35.0%; $Al_2O_3$, 27.0%; $Fe_2O_3$, 0.29%.

학회와 나-한국광산지질학회 편

김옥준,Kim, Ok-Jun 한국과학기술단체총연합회 1975 과학과 기술 Vol.8 No.12

부재자원개발과 한국의 우라늄

김옥준,Kim, Ok-Jun 한국과학기술단체총연합회 1976 과학과 기술 Vol.9 No.2

방사성 동위원소 우라늄 과학 ㆍ의학 ㆍ농업에 이용 토륨(Th) 매장량 풍부

동북아 안보전략의 변화와 북한 핵문제 북핵문제해결을 위한 중국의 적극적인 역할과 요인

김옥준 평화문제연구소 2004 統一問題硏究 Vol.16 No.1

With regard to the issue of North Korea``s nuclear weapon development program, China began to change its policy by voting for transfer of the North Korean issue to the Special Council of the IAEA of the Security Council of the UN. Since then, China has actively participated in the Tripartite Meeting and two Six Party Meetings. Furthermore, China persuaded North Korea to participate in the multilateral meetings to peacefully resolve the issue of North Korean nuclear weapon development by providing aid to North Korea. In this sense, this paper attempts to define the main factors that determined the active role of China on the North Korean issue by analyzing both domestic factors such as reform policy and new leadership of the Chinese government and international factors such as the Japan factor, Taiwan factor, Korean Peninsula factor, and North East Asian factor. In conclusion, China conceives the North Korean issue as an important issue on the North East Asian agenda that should be peacefully resolved by international cooperation. And the Chinese government believes that it should play an active role in the negotiations to achieve a dominant po sition in the North East Asian area.

서울 지하철(地下鐵) 부지일대(敷地一帶) 암석(岩石)의 암석학적(岩石學的) 및 암석역학적(岩石力學的) 기준설정(基準設定)을 위(爲)한 연구(硏究)

김옥준,이대성,정봉일,Kim, Ok Joon,Lee, Dai Sung,Jeong, Bong Il 대한자원환경지질학회 1984 자원환경지질 Vol.17 No.1

The object of this study is to offer the standarized data for the design and calculating engineering cost of the rock excavation an the construction of the 3rd and 4th Seoul Subway lines From Jnauary to March in 1983, this study was carried out by the both methods of the field and laboratary studies. In the field, the geological survey in the entire area of Seoul City and sites on the subway lines were carried out and also a site measure of uniaxial compressional strength of rock masses by using Schmidt hammer was done. The labartory studies were carsied out by a study of preuions surveyes, microscopic studies of the mineral composition and degree of weathering of rocks, and measure of uniaxial compressional strengths Finally an engineering classification of each rock masses of South Africa council for Scientific and Industrial Research, CSIR, after Bieniawski, 1974. was done. In this method of classification 6 parameters such as strength of intact rock material, rock quality designation, spacing of fractures, condition of fractures, groundwater conditions, and the effect of fracture strike and dip orientation in tunnelling were used to evaluate rating of each rock mass.

차령화강암(車嶺花崗岩) 저반(底盤)과 이에 관련된 금속광상(金屬鑛床)의 암석학적(岩石學的) 및 지질구조적(地質構造的) 연구(硏究)

김옥준,Kim, Ok Joon 대한자원환경지질학회 1977 자원환경지질 Vol.10 No.3

The Charyong batholith extends northeasterly from the west coast to the west of Wonju in the central parts of Korean Penninsula. The batholith is separated by the metamorphic complex into the northern and the southern granites. and is believed to intrude during the Daebo orogeny of early Jurassic to early Cretaceous age. It constitutes a sort of anticlinorium and the metamorphic complex can be regarded as a huge roof pendant. The modal analysis indicates that the Charyong batholith belongs to a series of adamellite-granodiorte-to-nalite. The oxidation property happened during a magmatic segregation reveals that the batholith shows in general orogenic assimilation trend. The granites of early to middle Jurassic age show orogenic assimilation trend, whereas those of late Jurassic to early Cretaceous age post orogenic noassimilation trend. The fracture system of the whole region is two folds: the fractures having attitute of $N25{\sim}40^{\circ}E$ and $70^{\circ}SE$ are regarded as tension fractures, and those of NS, and 50E to vertical and $N50^{\circ}E$ and $80^{\circ}E$ to vertical as shear fractures. All these facts suggest definitely that the Charyong batholith is the syntectonic intrusives during the Daebo orogeny. The mineral deposits in the area studied are gold-silver deposits in majority which was named by O,J.Kim(1970) as the Chonan metallogenic province. They are sulfides baring quartz veins which were emplaced along the tension and shear fractures originated by the Daebo orogeny.

옥천지향사대내(沃川地向斜帶內)에 분포(分布)하는 염기성암류(鹽基性岩類)의 암석학적(岩石學的) 연구(硏究)

김옥준,김규한,Kim, OK Joon,Kim, Kyu Han 대한자원환경지질학회 1976 자원환경지질 Vol.9 No.1

The basic rocks distributed in the Okchon paleogeosynclinal zone have been previously considered as intrusive in majority, but as sedimentary parensis in few variety. The present study is to find out some clues to conclude otherwise, if any, by clarifying 1) the nature and characteristics of the rocks, 2) type of the associated sedimentary rocks if any, and 3) their occurrence in related to regional geologic structure. The finding are as follows: 1) The basic rocks are identified and classified to hornblende gabbro, amphibolite, basalt and andesite (in part metamorphosed to meta-volcanics), green schist and peridotite(which appears in separate locality from the others). 2) Associated sedimentary rocks which appear to overlie the basic rocks are known as Kunjasan and Baekwhasan formations. The two formations are probably same, but been used differently by different authers at different localities. The rocks is exclusively consisted of cherty looking siliceous quartzite and some localitis it shows very calcarious nature. The formation seems to indicate a sort of pelagic siliceous sediments although it contain some pebbles. 3) The basic rock suites are always underlain by the same continuous, great thrust, which separates the Okchon paleogeosyncline zone from the neogeosynclinal zone in the area studied. The comparison of Okchon basic rocks suite to the ophiolite suites in other parts of the world indicates some similarity with which the writers suggested the probalility of Okchon basic rocks being ophiolites that occur along ancient geosuture line now represented by the great thrust.

상부(上部) 옥천층(沃川層)의 암석학적(岩石學的) 및 지구조적(地構造的) 해석(解釋)에 관(關)한연구(硏究)

김옥준,윤정수,Kim, Ok Joon,Yoon, Jeong Su 대한자원환경지질학회 1980 자원환경지질 Vol.13 No.2

In spite of the fact that the Okcheon system has been rather intensively studied by many geologists since 1945, it still remains as a controversal problem as to its stratigraphy and geologic age. Present study has mainly focused on the upper members of the Okcheon system, namely the Hwanggangri and the Kunjasan formations so as to clarify the lithology, the depositional environment and the tectonic evolution of the formations. The Kunjasan formation lying unconformably over the Hwanggangri formation which is supposed to be a meta-tillite is interpreted as a metamorphosed calcareous argillaceous and/or arenaceous sediments on contract to the idea postulated by some geologists that it was a derivative of silicified Hwanggangri formation. Lithology of the Kunjasan and the Hwanggangri formation is quite different in that the former is white in color, contains few pebbles, and mostly composed of diopside and detrital quartz, whereas the latter is black to dark in color, contains abundant and variable kinds of pebbles, and composed of more argillacous matrix that has been metamorphosed to hornfels. The Hwanggangri and the Kunjasan formations were deposited in the rather deep sea which has transgressed toward northeast from southwest in the late Precambrian time, and the writer (1970) had formerly designated it as Okcheon Paleogeosyncline. With the beginning of Paleozoic era, Okcheon neogeogyncline was formed to the northeast of the old paleogeogyncline area. The transgression of the sea had proceeded toward southwest in which Cambrian strata were accumulated. During this period the area occupied formerly by the paleogeosyncline was uplifted, so that most of the Hwanggangri and the Kunjasan formations were eroded away except in the area close to the neogeosyncline sea coast. This is the reason why the Hwanggangri and the Kunjasan formations are cropped out presently in the area of the vicinity of contact zone of the paleo- and neogeosyncline zones. The age of the Okcheon system has been reconfirmed to be Precambrian from the view of the facts that 1) the Hanggangri formation, the upper member of the Okcheon system is meta-tillite and correlated to the Precambrian tillite in the Yantze basin in China, 2) the Okcheon system has been moderately metamorphosed while other formations of the same age, if it is Paleozoic or later, have not been metamorphosed, and 3) tectonic history and limited areal distribution of the Hwanggangri and the Kunjasan formations is suggestive of Precambian age.