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네트워크 바이오 인증 기반 산업기술 유출방지 시스템에 관한 연구
이대성 한국융합보안학회 2011 융합보안 논문지 Vol.11 No.4
첨단기술을 보유하고 있는 기업이나 핵심정보를 처리하는 정보기관은 조직의 기밀이 유출되는 시점에서 막대한 경제적 손실은 물론, 치명적인 피해에 따른 조직의 존립 자체가 흔들리게 된다. 기존의 오프라인으로 유출되던 기밀정보는 최근 유비쿼터스 통신 환경을 기반으로, 다양한 장비를 통해 언제든지 네트워크를 통해 유출이 가능해졌다. 본 논문에서는 네트워크로 전송되는 기밀유출을 차단하기 위해 전송되는 모든 패킷에 대해 실시간으로 패킷을 인증하고 차단하는 통신 프로토콜을 제안한다. 특히, 기밀유출을 시도하는 사용자를 구분하기 위하여 전송되는 패킷마다 사용자 바이오 정보를 투명하게 삽입하는 기법을 제시한다. 또한, 실험을 통해 사용자 바이오 정보를 삽입하고 패킷마다 인증하더라도 효과대비 그 성능이 크게 저하되지 않음을 확인한다. Enterprise which has a core technology or organization which manages a core information will be walking into a critical situation like a ruins when organization's confidential information is outflowed. In the past confidential information that was leaked to the off-line, recently the outflow made possible through a variety of equipment at any time via the network based on theubiquitous communication environment. In this paper, we propose to authenticate and block all packets transmitted via the network at real-time in order to prevent confidentials outflow. Especially in or der to differentiate between users who attempt to disclose confidentials, we propose to insert user's biometric informaion transparently at per-packet basis, and also verify a performance by simulation
북한의 급변사태 시나리오 2 : 재스민혁명 국가들의 사례분석을 중심으로
이대성 한국융합보안학회 2017 융합보안 논문지 Vol.17 No.4
남유럽에서 시작된 민주화라는 물결은 남아메리카와 아시아로 확산되었고, 구소련과 동유럽을 붕괴시켰으며, 북아프리카와 중동지역 국가들에 재스민혁명이라는 모습으로 나타났다. 이로 인하여 다수의 학자들은 재스민혁명이 북한에도발생할 가능성이 있다는 조심스러운 전망을 하면서, 북한 급변사태와 관련된 연구들을 활발히 하여왔다. 이러한 연구의주제들은 급변사태의 발생원인과 시기, 그리고 주도세력 등에 초점이 맞추어졌고, 그 전개과정이 어떻게 될 것인가와 체제변화가 있을 것인가에 대한 논의는 부족하였다. 이에 본 연구에서는 재스민혁명 국가들의 체제변화를 분석한 결과에근거하여, 북한 급변사태 이후에 전개 가능한 시나리오를 Ⅰ유형 비교적 평화롭게 정권이 교체될 가능성, Ⅱ유형 분단된국가에서 통일된 이후에 다시 내전이 발생할 가능성, Ⅲ유형 정권이 교체된 이후에 김일성가계의 누군가가 재집권할 가능성, Ⅳ유형 정권교체는 성공하였지만 내전이 발생할 가능성, Ⅴ유형 정권교체도 실패하고 내전이 지속적으로 발생할가능성으로 분류하였다. The wave of democratization that started in southern Europe spread to South America and Asia, dismantling the Soviet Union and Eastern European countries and appeared as a Jasmine revolution in countries of North Africa and the Middle East. As a result, many scholars have actively carried out researches related to the sudden change of North Korea, while taking a cautious view that the Jasmine Revolution might occur in North Korea. The focuses of the studies were on the cause and timing of the sudden change and the main forces of the revolution in North Korea. There weren’t enough discussions on how the process will be developed and whether there will be a system change. In this study, based on the results of analyzing the systematic changes of the Jasmine revolution nations, it suggested five scenarios that can be developed after the sudden change of North Korea. Scenario type Ⅰ: Relatively peaceful and the possibility of regime change, Scenario type Ⅱ: Reunification and then civil war, Scenario type Ⅲ: Regime changed but one of Kim Il Sung family grabbing the power, Scenario type IV: Successful regime change but civil war happening, Scenario type V: Regime change failed and civil war continuing.
보은화강섬록암(報恩花崗閃綠岩) 서남부(西南部) 접촉대(接觸帶)에 관(關)한 암석학적(岩石學的) 연구(硏究)
이대성,박종심,Lee, Dai Sung,Park, Jong Sim 대한자원환경지질학회 1981 자원환경지질 Vol.14 No.2
Southwestern contact zone of the Boeun granodiorite occurs near the thrust fault between the Ogcheon Group and Majeonri Limestone Formation. Ogcheon Group, metasediments composed of the Munjuri Formation, Changri Formation, and unconformably overlying Hwanggangri Formation, belongs to greenschist facies of regional metamorphism accompanied with deformation of two fold axes, $N10^{\circ}E$ and $N45-65^{\circ}E$ directions. Basic metamorphic rocks occurring in the Changri and Limestone Formations are the meta-basalts and meta-diabases of tholeiitic basalt series. The meta-basalts intruded in the Changri Formation as sills, whereas the meta-diabases in the Changri and Limestone Formations as stocks in appearance. They are considered to have emplaced before the formation of two fold axes and related with the thrust fault, based on the geologic setting of the area. The metamorphic facies are identified to be greenschist facies to epidote-amphibolite facies for the meta-basalt, and epidote-amphibolite facies for the meta-diabases. It is interpreted that such a variety of facies was related from the combination of earlier deuteric alteration and later regional metamorphism. The metasediments in southwestern contact zont of the Boeun granodiorite which is a product of later syntectonic intrusion of middle Jurassic in age, show pyroxene-hornfels facies near the contact and amphibole-horenfels facies away from the contact to the mineral zoning in the contact metamorphic aureole of the Limestone Formation, based on the paragenetic analysis of mineral assemblages. The Limestone in the area appears to be considerably $SiO_2-CaO-MgO-CO_2-H_2O$ can be adopted to evaluate equilibrium conditions of the mineral assemblages in each mineral zone. It is revealed that a temperature gradient was existed accross the contact aureole ranging from the higher igneous side to lower sedimentary side, whereas no clear trend of $XCO_2$ variation appears but high mole fraction. The tremolite diopside-quartz-calcite assemblages occurs in common through the most mineral zones of contact aureole that is in good agreement with the equivalent reaction curve which extends over a wide range of $T-XCO_2$ conditions.
옥천지향사대(沃川地向斜帶)의 화성활동(火成活動)에 의한 광화작용(鑛化作用)의 유형(類型)에 관(關)한 연구(硏究)
이대성,지정만,이대운,Lee, Dai Sung,Chi, Jeong Mann,Lee, Dai Woon 대한자원환경지질학회 1980 자원환경지질 Vol.13 No.3
The granitic plutons associated with Ogcheon geosynclinal zone can be grouped into three different subzones; SE-Subzone for the migmatitic and schistose granites of the southeast margin, 101-181m.y. old; NW-Subzone for those of the northwest margin, 112-163m. y. old; and C-Subzone for those of central part of the zone, 63-183m.y. old. The intrusives in C-Subzone are further subdivided into the older, adamellite to granodiorite (148-183m.y. old) and the younger, perthitic granites (63-106m,y. old). The metallogenic distribution of South Korea suggests that, in the Ogcheon Zone, it is possible to delineate an elongated polymetallogenic province in the general orientation of the zone intimately related with the migmatite and plutonic zones mentioned. Moreover, the mineralization in the province was basically controlled by the patterns of local geology involving country rocks and related igneous bodies, that permit subdivision of the province into the following three parts: Northeast (NE) Province consists dominantly of thick Paleozoic calcareous sediments; Middle (M) Province is characterized by predominant argillaceous and partly calcareous sediments of Precambrian to Late Paleozoic age; and Southwest (SW) Province consisting mainly of volcanic and arenaceous sediments of Mesozoic age. The three different plutonic zones with three different country rock provinces above mentioned make a combination which consists of nine classes. Each class can be assumed to be characterized by specific mineralization type. In order to classify the mineralization types, the present study sampled twenty six ore deposits and mineralized areas in Ogcheon zone as shown figure 2; eight ore deposits from plutonic SE-Subzone, ten from the plutonic NE-Subzone and eight from the plutonic C-Subzone. The characteristics of the classes are as follows: NE-SE is predominant in Au-Ag vein and Sn-migmatite of katazonal occurrence; NE-C is most productive in Pb-Zn and remarkable in Fe contact deposit in mesozone and partly Pb-Zn-Cu skarn in limestone and subordinate in mesozone and partly Pb-Zn pipes; M-SE is considerable in Au-Ag vein and rare elements (Nb, Ta, etc.) of pegmatite; M-C is predominant in F-veins in epizone and Mo-W, Fe, Cu veins occur in replacement type; M-NW is productive in Fe metamorphic and skarn types, partly remarkable in Cu, Pb-Zn contact; SW-SE is barren in mineralization related to Jurassic igneous rocks; SW-C is predominant in alunite and pyrophyllite in tuffs; and SW-NW is scarece in Pb-Zn, Cu, As and Au-Ag veins.
괴산부근(槐山附近)에 분포(分布)하는 옥천층군(沃川層群)의 지질구조(地質構造)에 관(關)하여
이대성,김용준,채인철,Lee, Dai Sung,Kim, Yong Jun,Chai, In Chul 대한자원환경지질학회 1977 자원환경지질 Vol.10 No.4
This study is focused on the geological structure of Igog-Jangam folded zone in the vicinity of Goesan town where Ogcheon group distributes. The geology is composed of Gyemyungsan formation, Daehyangsan quartzite, Munjuri formation and Hwanggangri formation of Ogcheon group unknown age in descending order, and porphyritic biotite granite and dyke rocks that intruded into the Ogcheon group. The study revealed that Igog-Jangam folded zone is a plunged synclinal fold based on the following evidences; 1) Some pebbles in Hwanggangri formation at Minaemi-gol (a name of village) consists of phyllite of Munjuri formation. 2) The pebble bearing phyllitic bed in this area, Hwanggangri formation was recognized as the uppermost member in Ogcheon group instead of the basal one of the group. 3) A crest of anticlinal fold has been appeared near the Goegang bridge as a structural counter-part of that of the present area. 4) The study of lineation of minor fold in Munjuri formation also suggests that Igog-Jangam folded zone manifests to be a synclinal structure.
해남지역(海南地域)에 분포(分布)된 우항리층내(牛項里層內) 흑색(黑色)셰일의 유기지화학적(有機地化學的) 연구(硏究)
이대성,윤현수,Lee, Dai Sung,Yun, Hyun Soo 대한자원환경지질학회 1979 자원환경지질 Vol.12 No.4
The studied area occupies the southern part of Haenam peninsula located in the southwestern corner of Korea. The stratigraphic sequences of the area are grouped into following three units in ascending order. (1) Late Cretaceous sedimentary rocks of Uhangri Formation which consist of the alternative beds of black shales and tuffaceous sediments, Hwangsan acidic fine grained tuffs and Jindo rhyolite flows. (2) Late Cretaceous biotite granite and acidic porphyries which intruded the Late Cretaceous sedimentary rocks. (3) Tertiary(?) pitchstone. The study purposes to delineate any of geochemical aspects on the deposition of the sequences, the average amounts of organic materials and the effect to the maturation of hydrocarbonization which has been occured by the intrusives. Sixty nine black shale samples were collected from Uhangri Formation in the northern and southern coasts of the peninsula. Organic carbons, total extracted organic matters and hydrocarbons were mainly determined by the Soxhlet extraction method, together with C-H-N elemental analyses. Based on the field and laboratory studies, the following interpretations have been obtained. (1) The paleohydrostatic condition of the sedimentation which took place was relatively calm and stable to delineate a lacustrine environment. (2) The amounts of organic material were more or less constant throughout the period of the deposition of the sediments. (3) The degree of hydrocarbonization of the Uhangri Formation in the northern coast was taken place higher than that in the southern coast due to the differences of thermal effect by the biotite granite which is assumed to be as a heat source in the area. Among the northern coast, some black shales in Uhangri and Mogsam areas which had been under the most moderate temperature environment snow symptomatic oily material, whereas, those in Sinseongri area do not, which were presumably to be intensive thermal alteration by the later acidic porphyries.