포항-울산간의 점토자원의 지질과 그 물리화학적 특성에 관한 연구

김옥준,이하영,김서운,김수진,Kim, Ok Joon,Lee, Ha Young,Kim, Suh Woon,Kim, Soo Jin 대한자원환경지질학회 1971 자원환경지질 Vol.4 No.4

I. Purpose and Importance of the Study The purpose of the present study is to clarify to geological, mineralogical, and physico-chemical properties of the clay minerals deposits imbedded in the Tertiary sediments in the areas between. Pohang and Ulsan along southeastern coastal region of Korea. These clays are being mined and utilized for filter and insecticide after activation or simple pulverizing, nontheless activated clays are short coming as chemical industry in Korea has been rapidly grown in recent years. In spite of such increase in clay demand, no goological investigation on clay deposits nor physico-chemical properties of the clays have been carried out up to date. Consequently activated clays produced in Korea is not only of low grade but also of shortage in supply, so that Korea has to import activated clays of better grade. The importance of the present study lies, therefore, on that guiding principle could be laid down by knowing stratigraphical horizons, of clay deposits and fundamental data of improving grade of activated clays might be derived from the results of physico-chemical examinations. II. Contents and Scope of the study The contents of the study are pinpointed down in the following two subjects: 1) General geological investigation of Tertiary formations distributed in the areas between Pohang and UIsan, and detail geological study of the bentonitic clay deposits imbedded in them. 2) To clarifty physico-chemical characteristics of the clays by means of chemical analysis, X-ray diffraction and electron microscope. The scope of the study involves the following there points: i) Regional geological investigation-This investigation has been carried out in order to find out the distribution of Tertiary sediments and exact location of clay mineral deposits in the areas between Pohang and UIsan. ii) Detail geological investigation-This has been concentrated in and around the clay deposits which. had been found out by the regional investigation. iii) Laboratory researchs include i) age determination and correlation of Tertiary sediments by paleontological study, and ii) Chemical analysis, X-ray diffraction, and electron microscopic studies on clays, samples taken from various clay deposits. III. Research Results and Suggestions 1) The geology of the area investigated is composed mainly of Janggi and Beomgokri groups of Miocene age in ascending order rested on the upper Silla system, Balkuksa granite and volcanic rocks of upper Cretaceous age as base. 2) Janggi group is composed in ascending order of Janggi conglomerate, Nultaeri rhyolitic tuff, Keumkwangdong shale, two beds of lignite-bearing formations which consist of alternation of conglomerate, sandstone and mudstone, and andesitic, rhyolitic, and basaltic tuff beds. 3) Beomgokri group is mainly composed of andesitic to rhyolitic tuff interlayered by conglomerate and tuffaceous sandstone. In the areas around boundary between North-and South Kyeongsang-do is distributed Haseori farmation which is composed of conglomerate, sandstone, mudstone and andesitic to rhyolitic tuff, and which is correlated to Eoilri formation of Janggi group. 4) Clay deposits of the area are interbedded in Eoilri, Haseori, Nultaeri tuff, Keumkwangdong shale, upper and lower horizon of the lower lignite-bearing seam, and Keumori rhyolitic tuff formations of Janggi group; and are genetically classi.fied into four categories, that is, i) those derived from volcanic ash beds(Haseori and Daeanri deposits), ii) those of secondary residual type from rhyolitic tuff beds(Seokupri deposits), iii) Clay beds above and beneath the lignite seams, (Janggi and Keumkwangdong deposits), and iv) those derived from rhyolitic tuff beds(Sangjeong and Tonghae deposits). 5) Mineral constituents of clay deposits are, according to X-ray diffraction, montmorillonite accompanied in different degree by cristobalite, plagioclase, quartz, stilbite, and halloysite in rare occasion. The clays are grouped according t

제천군(提川郡) 하천리(荷川里)-월굴리(月窟里) 지역(地域)의 지질구조(地質構造)와 암석학적(岩石學的) 연구(硏究)

김옥준,유강민,Kim, Ok Joon,Yu, Kang Min 대한자원환경지질학회 1977 자원환경지질 Vol.10 No.1

The study area is located in between Hacheonri and Weolgulri, Jecheon-gun where the formations of Okcheon group and Chosun group come in contact and the stratigraphy and geological age of the Okcheon group have been debated among previous workers. The dolomitic limestone which distributed at Cheongam and Dumusil is clarified as the Hyangsanri dolomite formation and the quartzite distributed at Cheongam and Howeunri as Taehyangsan quartzite formation. The newly named Soorumsan schist interbedded in the Great Limestone Series was previously classified Seochangri formation. It is also classified that the formation formerly named as Seochangri was divided into newly named Manji schist which seems to be correlated to Kemyeongsan and Munjuri formation. The formation formerly named as Buknori is clarified as Hwanggangri formation. The Samtaesan formation has been clarified as the lower and upper limestone beds which belong to the Great Limestone Series. The area divided into two groups, that is, Okcheon system of Pre-cambrian age occupies western part and the Great Limestone Series of Chosun system of Cambro-Ordovician age eastern part of this area. Okcheon system consists in ascending order of Manji schist, Hyangsanri dolomite, Taehyangsan quartzite, Munjuri schist, and Hwanggangri formation of meta-tillite. The Great Limestone Series of Chosun group consists in ascending order of lower limestone, Soorumsan schist, Hoosanri quartzite and upper limestone formations. Busan augen gneiss seems to be igneous origin. Unmetamorphosed shale interbed can be traced in the Soorumsan schist. Previous study (Kims, 1974) reveals that meta-volcanic rocks are distributed from south to north along contact zone of the Okcheon and Chosun groups, and it has been confirmed that the meta-volcanics crop out continuously from the adjacent southern quardrangle into the southern part of the area studied, intruding along the fault zone between the Okcheon and Chosun groups which seems to be upthrust as in the area south. This evidence coincides with Kims' work (1974) which states that the Precambrian Okcheon group is largely overturned and thrusted over the Chosun group.

수산리(水山里)-황강리지역(黃江里地域)의 지질구조(地質構造)와 암석학적(岩石學的) 연구(硏究)

김옥준,김규한,Kim, Ok Joon,Kim, Kyu Han 대한자원환경지질학회 1974 자원환경지질 Vol.7 No.3

The study area is located in between Susanri and Hwanggangri where the formations of Okcheon group and Chosun group supposedly come in contact so that the area is structurally very import. Present study reveals that the meta-volcanic rocks distribute from south to north along contact zone of Okcheon and Chosun groups in the center of the area. Meta-volcanic rocks seem to be originated from the andesite or andesitic basalt rocks which was known to be Surchangri formation consist of phyllite and black slate by previous workers. The meta-volcanic rocks intruded along the fault zone one existed between Okcheon and Chosun groups but obliterated at present by the intrusion of volcanic rocks. The fault seems to be overthrust, and one of the positive evidences of thrust fault is the Yamisan nappe structure in Yamisan near Susanri. This interpretation coincides with O.J. Kim's work which states that the Precambrian Okcheon group is largely overturned and thrusted over the Chosun group. The relation between the Surchangri and the Majeonri formation marks facies change. This fact together with northpluging anticlinal structure made it possible that both formation came into contact along direction without fault. Yongam formation is not overlain unconformably used to be believed by previous workers, but interbed in the Great Limestone series of Chosun goup. It is also clarified that the rock formerly designated as limesilicate rock was meta-liparite. The origin of amphibole pebbles in the Kunjasan formation is of primary and secondary ones; the secondary pebbles were formed by metamorphism of the fragments of limestone or dolomite.

提川郡 荷川里-月窟里 地域의 地質構造와 岩石學的 硏究

Ok Joon Kim(金玉準),Kang Min Yu(兪剛民) 대한자원환경지질학회 1977 자원환경지질 Vol.10 No.1

The study area is located in between Hacheonri and Weolgulri, Jecheon-gun where the formations of Okcheon group and Chosun group come in contact and the stratigraphy and geological age of the Okcheon group have been debated among previous workers. The dolomitic limestone which distributed at Cheongam and Dumusil is clarified as the Hyangsanri dolomite formation and the quartzite distributed at Cheongam and Howeunri as Taehyangsan quartzite formation. The newly named Soorumsan schist interbedded in the Great Limestone Series was previously classified Seochangri formation. It is also classified that the formation formerly named as Seochangri was divided into newly named Manji schist which seems to be correlated to Kemyeongsan and Munjuri formation. The formation formerly named as Buknori is clarified as Hwanggangri formation. The Samtaesan formation has been clarified as the lower and upper limestone beds which belong to the Great Limestone Series. The area divided into two groups, that is, Okcheon system of Pre-cambrian age occupies western part and the Great Limestone Series of Chosun system of Cambro-Ordovician age eastern part of this area. Okcheon system consists in ascending order of Manji schist, Hyangsanri dolomite, Taehyangsan quartzite, Munjuri schist, and Hwanggangri formation of meta-tillite. The Great Limestone Series of Chosun group consists in ascending order of lower limestone, Soorumsan schist, Hoosanri quartzite and upper limestone formations. Busan augen gneiss seems to be igneous origin. Unmetamorphosed shale interbed can be traced in the Soorumsan schist. Previous study (Kims, 1974) reveals that meta-volcanic rocks are distributed from south to north alone contact zone of the Okcheon and Chosun groups, and it has been confirmed that the meta-volcanics crop out continuously from the adjacent southern quardrangle into the southern part of the area studied, intruding along the fault zone between the Okcheon and Chosun groups which seems to be upthrust as in the area south. This evidence coincides with Kims’ work (1974) which states that the Precambrian Okcheon group is largely overturned and thrusted over the Chosun group.

중국의 한국전 참전에 대한 전략적 고려

김옥준(Kim Ok-Joon) 동아시아국제정치학회 2013 국제정치연구 Vol.16 No.1

China has almost no intention to participate in the Korean war in its early phrase. This intention had been changed by the involvement of the formidable American military forces. This study examines how the Chinese perception of the war involvement developed as the war situation changed. Through this analysis it evaluates several issues and disagreements related to the Chinese participation decision; First, China had prepared to participate into the war in the very beginning of the North Korean preparation. Second, the Chinese decision was materialized after the American forces became involved. Third, the Chinese government insisted that the assistant of the Soviet air force should be a precondition for its war participation. Fourth, the decision was made in the middle of August when the war appeared to be dragged for long. To properly evaluate these issues this study covers the period from the start of the war to Kim’s request for Chinese war participation on Semester in 1950.

옥천대(沃川帶)의 지질(地質) 및 광물자원(鑛物資源)에 관(關)한 연구(硏究) -평창(平昌)~영월(寧越)~제천지역(堤川地域)의 지질구조(地質構造)-

김옥준,박봉순,민경덕,Kim, Ok Joon,Park, Pong Soon,Min, Kyung Duck 대한자원환경지질학회 1985 자원환경지질 Vol.18 No.4

The geological structures and some of the stratigraphy in the area studied are being thought to be ambiguous and controvertible. The present study intended to clarify these ambiguities by correct interpretation of the geological structures and lithostratigraphy of the area concerned. The so-called "Sambangsan formation", which was designated as an unknown age by the Taebaksan Geological Investigation Corps (1962) and as the mid Cambrian age by T. Kobayashi (1966) and I.S. Kim (1983), has been determined by the present study as the $Hongj{\breve{o}}m$ series of Carbo-Permian age resting unconformably on the Cambro-Ordovician limestone formations. This determination was supported by conodont study concurrently carried out by I.S.Kim. The so-called "Daehari formation", which was renamed by the later study group after the original "Sambangsan formation" distributed in the area from southwest of Sambangsan toward southwest to $Juch{\breve{o}}n$, possesses more or less the same lithlogy as "Sambangsan formation" of the old designation in the eastern of the area, but different lithology in the western localities where Sadong formation, the basal sandstone member of the Kobangsan formation and the green shale member of the Nokam formation are cropped out. The narrow belt of the complex mixture of the $Py{\breve{o}}ngan$ group in-between limestone formations extending over 16km with a width of 500m to 1000m was formed by the faults: the northern boundary with the limestone formations is a fault contact all the way through entire area and the southern boundary is either fault contact in most of the area and unconformity in some other area. The $Hongj{\breve{o}}m$ formation on the Mt. Sambangsan shows rather steeply dipping nearly isoclinal folds which plunges $10^{\circ}$ to $20^{\circ}$ southward. There are also field evidences that the limestone formations distributed in both north and south of the Hongjom formation (erstwhile "Sambangsan formation") along the Sambangsan ridge are the same formations and show the same folding as the $Hongj{\breve{o}}m$ formation. Therefore, these limestone formations should be rezoned in the light of the new structural interpretation although they were differently designated in the previous studies as $Py{\breve{o}}ngchang$ and $Y{\breve{o}}ngw{\breve{o}}l$-type of the Joson Group. The structures developed in the area mostly faults, which acted as one of the guides for the new interpretation of the geology and structure of the area are described and shown on the geologic map.

북한의 남침에 대한 중국의 지원약속과 소련의 역할: 북한의 남침제의부터 남침개시 전까지를 중심으로

김옥준 ( Ok Joon Kim ) 대한정치학회 2011 大韓政治學會報 Vol.18 No.1

본고에서는 위에서 언급한 김일성의 남침제의에서부터 남침개시 전까지 기간동안의 시간적인 범위, 즉 김일성의 남침제의에 대한 거부에서 승인으로 전환되는 과정에서의 스탈린의 전략적 계산 및 마오의 지원약속 배경과 의미 등을 중점적으로 살펴보고자 한다. 특히 쟁점이 되고 있는 스탈린이 김일성의 남침을 승인하는 과정에서 미군의 직접개입에 관한 고려, 그리고 김일성의 남침제의와 지원에 대한 마오의 입장, 인민해방군 조선인부대의 북한인도, 미군의 개입가능성 평가, 인민해방군 재배치의 의미 등을 중점적으로 분석한다. 미국과의 직접충돌을 우려하고 있었던 스탈린에게 단서가 있었지만 중국의 직접파병 약속은 김일성의 남침계획을 승인하는데 결정적인 작용을 하였으며, 스탈린은 끝까지 김일성의 남침계획의 전면에 나서지 않으면서 이 전쟁에 중국을 끌어들였다. 미군의 직접개입 가능성을 낮게 평가한 마오는 스탈린의 전략에 휘말려 들어갔으며 결국 전쟁 발발 후 며칠이 지나지 않아 마오의 판단은 빗나가고 말았다. This study mainly examines factor that affected Stalin`s strategic calculations and decisions on the Korean war and Mao`s commitment to support North Korea`s war efforts in the period stretching from Kim Il Sung`s invasion proposal to the initiation. A particular focus is given to the issue how Stalin`s concern with the direct involvement of the US Army with the Korean war affected his decision of Kim`s proposal. Other interesting issues include Mao`s attitude of Kim`s proposal, the transfer of Korean Liberation Army soldiers to North Korea, the possibility of American intervention, and the significance of the relocation of the People`s Liberation Army. Stalin, who was concerned with direct confrontations with the US, approached the matter cautiously. Yet the Chinese promise of military engagement prompted his approval. Stalin had been behind the scene and succeeded in drawing the Chinese involvement. On the other hand, Mao underestimated the possibility of the US involvement and was entangled with the war shortly. The process of the war in a few days proved that Mao was wrong.

Distribution of Aquaporins (Water Channels) in the Rat Salivary Glands

정지연(Ji-Yeon Jung),한창룡(Chang-Ryoung Han),정연진(Yeon-Jin Jeong),오원만(Won-Mann Oh),김미원(Mi-Won Kim1),김선헌(Sun-Hun Kim),김옥준(Ok-Joon Kim),김현진(Huyn-Jin Kim),고정태(Jeong-Tae Koh),최홍란(Hong-Ran Choi),김원재(Won-Jae Kim) 대한해부학회 2002 Anatomy & Cell Biology Vol.35 No.3

침샘은 하루 1.5 l의 침을 분비하며, 일반적으로 침샘에서 수분이동은 능동적 염분 이동에 따른 삼투현상에 의해 일어난다. 따라서 침샘에서 높은 수분투과성으로 인해 수분통로 단백인 aquaporin (AQP)들이 풍부하게 존재할 수 있다. 지금까지침샘에 4가지 형태의 AQP이 존재한다고 알려져 있지만 침샘에서 정확한 위치와 수분 이동에 대한 각 AQP들의 역할은 아직 확실치 않다. 본 연구는 300 g 정도의 흰쥐를 pentobarbital sodium (50 mg/kg, IP) 마취하에서 carbarchol (10 μg/kg)을 복강 내 투여한 후 AQP들의 역할과 분포를 면역조직화학방법으로 조사하였다. AQP1은 침샘의 미세혈관의 내피세포와 샘세포와 샘관 주위에 존재하는 근육상피세포에 존재하였다. AQP4는 침샘관의 마지막 부위인 배출관에 존재하였다. AQP5는 주로 장액세포의 바닥가쪽과 세포사이 분비소관을 포함한 세포꼭대기쪽막 에 존재하였으며 콜린성 분비 자극으로 세포꼭대기쪽막으로 이동되어 밀집되었다. AQP5는 모든 침샘의 사이관과 줄무늬 관에도 존재하였으며 점액세포는 약하게 존재하였다. AQP8은 AQP5처럼 장액세포의 바닥쪽막과 세포사이 분비소관을 포함한 세포꼭대기쪽막에 존재하였으며 콜린성 침분비 자극으로 세포꼭대기쪽막쪽으로 이동되어 밀집되었다. 이상의 실험결과는 AQP5와 AQP8이 장액세포에서 일차 침 형성시 일어나는 수분이동의 주된 통로임을 시사하였다. The salivary glands produce 1.5 l of fluid per day. As in other organs, the general paradigm in the salivary glands is that water movement occurs secondary to osmotic driving forces created by active salt transport. Therefore, high water permeability in salivary glands is expected to need a variety of aquaporin (AQP), a water channel. Although four AQPs have been known to reside in salivary glands, the precise location and roles of AQPs have been not well examined. This study is aimed to investigate the distribution of AQPs in 3 major salivary glands and their changes after cholinergic stimulation using immunohistochemical study in Sprague Dawley rats weighing 300 g under pentobarbital sodium anesthesia. AQP1 was localized in the endothelial cells of all salivary capillary vessels and the myoepithelial cells. AQP4 was demonstrated in the epithelium of the excretory ductal cells of all salivary glands. AQP5 and 8 were abundantly present in the basolateral membrane and apical membranes of the serous acini including intercellular secretory canaliculi, whereas AQP5 was weakly present in mucous acini. In addition, AQP5 was found in the epithelium of the intercalated and striated ducts. Upon stimulation of carbachol (10 μg/kg, I.P). AQP5 and 8 tended to translocate from basolateral membrane to the apical membrane, appearing as clusters of dots. These results suggest that AQP5 and 8 are the candidate molecules responsible for the water movement in salivary acinar cells.

Granites and Tectonics of South Korea

김옥준,Kim, Ok Joon The Korean Society of Economic and Environmental G 1975 자원환경지질 Vol.8 No.4

남한(南韓)은 지구조적(地構造的)으로 4개의 지질구(地質區)로 나누어 진다. 경기육괴(京畿陸塊)와 영남육괴(嶺南陸塊)는 선(先)캠브리아기(紀)의 편마암(片麻岩)과 편암(片岩)으로 구성되어 있다. 결천지향사대(決川地向斜帶)는 소위 지나방향(支那方向)인 서남남동(西南南東)으로 한반도(韓半島)를 비스듬히 가로지르고 있다. 옥천지향사대(沃川地向斜帶)의 북동부(北東部)는 주(主)로 고생대(古生代)와 중생대(中生代) 초기의 퇴적암층(堆積岩層)으로 되어있고 서남부(西南部)는 후기 선(先)캠프리아기(紀)의 변성암층군(變成岩層群)으로 되어있다. 경상분지는 백악기(白堊紀)의 두꺼운 육성퇴적층(陸成堆積層)과 안산암류(安山岩類)로 되어있다. 제3기(第三紀)의 몇 개의 소분지(小盆地)가 한반도 동남부와 제주도에 분포(分布)하고 주로 해성층(海成層)과 현무암류로 되어있다. 쥬라기(紀)의 대보화강암(大寶花崗岩)이 경기육괴(京畿陸塊), 영남육괴(嶺南陸塊), 결천지향사대내(決川地向斜帶內)에 지나방향(支那方向)으로 관입분포(貫入分布)한다. 한편 백악기(白堊紀)의 불국사(佛國寺) 화강암(花崗岩)은 경상분지에 분산분포(分散分布)한다. South Korea is divided tectonically into four segments. The Kyonggi-Ryongnam massif is composed of Precambrian schists and gneisses and consititutes a base for the succeeding formations. The Okcheon geosynclinal zone in the Kyonggi-Ryongnam massif strectches from southwest to northeast diagonally across the peninsula in a direction known as the Sinian direction. Its northeastern part is composed primarily of Paleozoic to early Mesozoic sedimentary formations and the southwestern part of the late Precambrian Okcheon metamorphic series. The Kyongsang basin occupies the southeast and southwest of the peninsula and is made up of a thick series of Cretaceous terrestrial sedimentary and andesitic rocks. A few small Tertiary basins are scattered in the eastern coastal area and in Cheju Island, and are composed of marine sedimentary and basaltic rocks. Jurassic Daebo granites intrude the Kyonggi-Ryongnam massif and the Okcheon zone in the Sinian direction, whereas late Cretaceous Bulkuksa granites are scattered randomly in the Kyongsang basin.

남한(南韓) 대석회암통(大石灰岩統)의 층서(層序)와 지질구조(地質構造)

김옥준,이하영,이대성,윤석규,Kim, Ok Joon,Lee, Ha Young,Lee, Dai Sung,Yun, Suckew 대한자원환경지질학회 1973 자원환경지질 Vol.6 No.2

The purpose of the present study is to clarify the stratigraphy and geologic structure of the Great Limestone Series by means of study on fossil conodonts and detail investigation of geologic structure. In recent years very few geologists in Korea argue without confident evidences against the age and stratigraphy of the Great Limestone Series which have been rather well established previously in most parts of the regions although it is ambiguous and has not been studied in other areas. Five type localities in the Kangweon basin where the Great Limestone Series is well cropped out were chosen for the study. Total 26 genus and 66 species of conodont were identified from 290 samples collected and treated. From the study on conodonts the age of each formations of the Great Limestone Series has been determined as follows: The Great Limestone Series of Duwibong type Duwibong limestone: Caradocian (mid-Ord.) Jikunsan shale: Landeilian (mid-Ord.) Maggol limestone: Llanvirn-Llandeilian (mid-Ord.) Dumugol: Arenigian (Ord.) Hwajeol: Upper Cambrian The Great Limestone Series of Yeongweol type Mungok (Samtaesan) : Ordovician Machari: upper Cambrian The Great Limestone Series of Jeongseon type Erstwhile Jeongseon limestone: mid-Ord. The erstwhile Jongseon Limestone formation in Jeongseon district is separated into Hwajeol, Dongjeom, Dumudong, and Maggol formations which were cropped out repeatedly by folding and faulting, but Maggol is predominant in areal distribution. Yemi Limestone Breccia bed is not a single bed but distributed in several horizons so that it bears no stratigraphic significance. The limestone bed above Yemi Limestone Breccia, which was believed by some geologists to be much younger than Ordovician, is identified to be Maggol and its age is determined to be mid-Ordovician. Sambangsan formation in Yeongweol district was believed to be Cambrian age and lower horizon than Machari formation by Kobayashi, but C. M. Son believed that it might belong to later than Ordovician and lies above the Great Limestone Series of Yeongweol type. It was identified to be upper Cambrian and lies beneath the Machari formation and above the Daeki formation, the lower most horizon of the Great Limestone Series. The age of Yeongweol type Choseon system is contemporaneous with that of Duwibong type Choseon system. The difference in lithofacies is not due to lateral facies change, but due to the difference in its depositional environment. The Yeongweol type Choseon system is believed to be deposited in the small Yeongweol basin which was separated from the main Kangweon sedimentary basin. Judging from these facts it is definitely concluded that there exists no Gotlandian formation in the regions studied. Structurally the Kangweon basin comprises five basins and two uplifted areas. These structures were originated by at least two crustal movements, that is, Songrim disturbance of Triassic and Daebo orogeny of Jurasic age.