RISS 학술연구정보서비스

검색
다국어 입력

http://chineseinput.net/에서 pinyin(병음)방식으로 중국어를 변환할 수 있습니다.

변환된 중국어를 복사하여 사용하시면 됩니다.

예시)
  • 中文 을 입력하시려면 zhongwen을 입력하시고 space를누르시면됩니다.
  • 北京 을 입력하시려면 beijing을 입력하시고 space를 누르시면 됩니다.
닫기
    인기검색어 순위 펼치기

    RISS 인기검색어

      검색결과 좁혀 보기

      • 좁혀본 항목

      • 좁혀본 항목 보기순서

        • 원문유무
        • 음성지원유무
          • 원문제공처
          • 등재정보
          • 학술지명
          • 주제분류
          • 발행연도
          • 작성언어
          • 저자

        오늘 본 자료

        • 오늘 본 자료가 없습니다.
        더보기
        • 무료
        • 기관 내 무료
        • 유료
        • KCI우수등재

          제도적 논리와 조직정치, 그리고 조직의 균형전략: 성과주의 인사제도의 제도화 과정을 중심으로

          최선규 한국사회학회 2019 韓國社會學 Vol.53 No.3

          An institutional environment is composed of multiple stakeholders, each with different interests, values, and purposes. Therefore, the process of introduction and diffusion of new human resource management systems involves conflicts and struggles between stakeholders who stick to an old institutional logic and stakeholders who advocate a new one. In this study, based on institutional logic, I examined how the demands of pluralistic stakeholders with different interests and goals impact on the institutionalization of performancebased human resource management(hereinafter called “P-based HRM”). And it investigated how organizations respond to the conflicting demands of an institutional stakeholders. To this end, the study used data from the Third Wave (2009) to the Fifth Wave (2013) of the Human Capital Corporate Panel (HCCP) of the Korea Research Institute for Vocational Education and Training and analyzed it with a panel multinominal logit model. The results are as follows. First, the study found that the larger the size of the human resources department of an organization intensifies the adoption of the P-based HRM. On the other hand, it is found that a labor union has a negative impact on the intensity of adopting the P-based HRM. Second, it is expected that the more reinforced that P-based HRM which stresses a linkage between performance and graded compensations, the greater the tension between the labor union and human resource managers. Thus, this study analyzes the relationship between the intensity of the P-based HRM and the type of strategy for reflecting graded incentives. As a result, it is found that organizations which introduce and operate both an Yeonbongje and management by objectives (MBO) are more likely to select a balancing strategy that keeps a proper ratio reflecting individual-based incentives and group-based incentives than other organizations. These results suggest that the institutionalization of P-based HRM can be perceived as the process that each stakeholder political struggle for enhancing their status, power and legitimacy within the organization. Also, this study shows that organizations flexibly and strategically respond to the pressures of pluralistic, complex institutional environment for the legitimacy, resources, and internal stability, which are essential for an organization to survive. 제도적 환경은 서로 다른 이해와 가치, 목적을 가진 이해관계자들로 구성되어 있다. 따라서 새로운 제도의 도입과 확산 과정에는 기존의 제도를 고수하는 이해관계자와 새로운 제도를 지지하는 이해관계자들 사이에 갈등이나 투쟁이 수반된다. 본 연구에서는 제도적 논리를 토대로 서로 다른 이해와 목적을 지닌 다원적인 이해관계자들의 요구가 성과주의 인사제도의 제도화 과정에 어떠한 영향을 미치는지를 규명하였다. 그리고 상충하는 이해관계자의 요구에 노출된 조직이 어떠한 방식으로 대응하는지 살펴보았다. 이를 위해, 한국직업능력개발원의 인적자본기업패널 3차년도(2009년)~5차년도(2013년) 자료를 활용하여 패널 다항 로짓 모형으로 분석하였다. 연구결과는 다음과 같다. 먼저 인사부서의 규모가 클수록 성과주의 인사제도 도입 강도를 강화하는 것으로 나타난 반면, 노동조합은 성과주의 인사제도 도입 강도에 부정적인 영향을 미치는 것으로 나타났다. 다음으로, 성과와 차등적 보상 사이의 연계를 강조하는 성과주의 인사제도 운영이 강화될수록 노동조합을 비롯한 내부 구성원과 인사부서 사이의 갈등은 커질 것으로 예상하여, 성과주의 인사제도 운영강도와 차등 성과급 반영 전략 유형 사이의 관계를 분석하였다. 분석의 결과, 연봉제와 목표관리제를 모두 도입하여 운영하는 조직일수록 그렇지 않은 조직에 비해 개인 성과급과 집단 성과급반영 비중을 적절하게 유지하는, 즉 균형전략을 선택하는 것으로 나타났다. 이러한 연구결과는 성과주의 인사제도의 도입과 확산을 각 이해관계자들이 자신의 지위나 권력을 강화하거나 정당성을 확보하기 위한 정치적 투쟁의 과정으로 접근할 필요성을 시사하고 있다. 그리고 조직은 생존에 필수적인 정당성과 핵심 자원, 조직의 안정성을 고려하여 상충하는 이해관계자들의 요구에 전략적으로 대응할 수 있는 행위자임을 보여주고 있다.

        • KCI등재

          충청도(忠淸道) 일원(一圓)의 금(金)·은(銀)광상(鑛床)에 대한 광물학적(鑛物學的) 연구(硏究)

          최선규,박노영,홍세선,Choi,,Seon,Gyu,Park,,No,Young,Hong,,Sei,Sun 대한자원환경지질학회 1988 자원환경지질 Vol.21 No.3

          A large number of gold and/or silver-bearing quartz veins occur in or near Mesozoic granite batholith elongated in a NE-SW direction within the Chungcheong Province. Precambrian schists and gneisses, and Jurassic and Cretaceous granitic rocks serve as hosts for gold and/or silver deposits. On the basis of Ag/Au total production and ore grade ratio, 15 mines may be divided into three major groups: gold-dominant deposits, gold-silver deposits, and silver-dominant deposits. The chemical composition of electrum from skarn deposit (Geodo mine), alaskite-type deposit (Geumjeong mine) and 15 vein deposits was summarized. It was found that the Au content of electrum for vein deposits ranging from 5.2 to 86.5 is lower than that for skarn and alaskite deposits. Among 15 vein deposits, the composition of electrum associated with pyrrhotite is relatively high and has a narrow range of 40.8 to 86.5 atomic % Au, but the Au content of electrum with pyrite is in range of 5.2 to 82.8 atomic %, and is clearly lower than that with pyrrhotite. The grouping of ages for these mines indicates that gold and/or silver mineralizations occurred during two periods in the Mesozoic. Daebo igneous activities are restricted to gold mineralization in the range of 158 to 133 Ma, whereas Bulgugsa igneous activities are related to gold and/or silver mineralization ranging from 108 to 71 Ma. Generally speaking, Jurassic gold-dominant veins have many common characteristics; notably prominent association with pegmatites, simply massive vein morphology, high fineness in the ore concentrates, rarity of silver minerals, and a distinctively simple mineralogy, including sphalerite, galena, chalcopyrite, pyrrhotite and/or pyrite. Although individual deposits exhibit widely differing diversity, Cretaceous gold-silver and silver-dominant veins are characterized by features such as complex vein, low to medium fineness in the ore concentrates and abundance of silver minerals including Ag sulfosalts, Ag sulfides, Ag tellurides and native silver.

        • KCI등재SCOPUS

          Relationship Between Obesity and N-Terminal Brain Natriuretic Peptide Level as a Prognostic Value After Acute Myocardial Infarction

          최선규,정명호,안영근,조정관,강정채,채성철,허승호,홍택종,김영조,성인환,채제건,류재영,채인호,조명찬,배장호,나승운,김종진,최동훈,장양수,윤정한,정욱성,승기배,박승정,Other,Other,KAMIRI,Investigators 대한심장학회 2010 Korean Circulation Journal Vol.40 No.11

          coronary syndrome has been demonstrated in many studies. However, NT-proBNP levels are influenced by various factors such as sex, age, renal function, heart failure severity, and obesity. NT-proBNP concentrations tend to decrease with higher body mass index (BMI). The aim of this study was to examine the influence of obesity on NT-proBNP as a predictive prognostic factor in acute myocardial infarction (AMI) patients. Subjects and Methods: Using data from the Korea Acute Myocardial Infarction Registry (January 2005 to September 2008), 2,736 AMI patients were included in this study. These patients were divided into men (n=1,972, 70%) and women (n=764, 30%), and were grouped according to their BMIs. Major adverse cardiac events (MACE) during 1 year clinical follow-up were evaluated. Results: NT-proBNP was significantly higher in lower BMI (p<0.001). Mean NT-proBNP levels of each obesity group were 2,393±4,022 pg/mL in the lean group (n=875), 1,506±3,074 pg/mL in the overweight group (n=724) and 1,100±1,137 pg/mL in the obese group (n=1,137) (p<0.01). NT-proBNP was an independent prognostic factor of AMI in obese patients by multivariative analysis of independent risk factors of MACE (p=0.01). Conclusion: NT-proBNP is lower in obese AMI patients than in non-obese AMI patients, but NT-proBNP is still of independent prognostic value in obese AMI patients.

        • KCI등재

          한국 중부와 동남부지역 금은 광화작용의 성인적 특성

          최선규,최상훈 대한자원환경지질학회 1995 자원환경지질 Vol.28 No.6

          '스콜라' 이용 시 소속기관이 구독 중이 아닌 경우, 오후 4시부터 익일 오전 7시까지 원문보기가 가능합니다.

        • KCI등재

          한국 중부지역 금은광상산 섬아연석의 조성변화와 성인적 특성

          최선규,Choi,,Seon-Gyu 대한자원환경지질학회 1993 자원환경지질 Vol.26 No.2

          '스콜라' 이용 시 소속기관이 구독 중이 아닌 경우, 오후 4시부터 익일 오전 7시까지 원문보기가 가능합니다.

          Chemical compositions of sphalerites from 25 gold and/or silver deposits in central Korea were obtained with an electron probe microanalyzer. The FeS contents of sphalerites depend generally upon the assemblage of associated iron sulphides (pyrite and/or pyrrhotite) especially. The sphalerites coexisting with pyrrhotite show a narrow range of FeS variation, but the sphalerites associated with pyrite and/or pyrrhotite have the variable and wide range of FeS contents. The sphalerites from Au-dominant deposits, which vary considerably in each deposit, are generally characterized by high CdS content and low MnS content. On the contrary, the sphalerites from Ag-dominant and Au-Ag deposits tend to be characterized by relatively high MnS and very low CdS content. Based upon the mineralogy, fluid inclusions and stable isotope data, the Au-dominant deposits were formed under higher temperature and deeper depth than the Ag-dominant and Au-Ag deposits. The results suggest the possibility that the diverse sources and evolution of ore fluid at the time of ore deposition are responsible for the deposition of Cd and Mn components in sphalerites.

        • KCI등재

          한국 금-은 광상의 효율적 탐사를 위한 성인모델;무극 광화대를 중심으로

          최선규,이동은,박상준,최상훈,강흥석 대한자원환경지질학회 2001 자원환경지질 Vol.34 No.5

          '스콜라' 이용 시 소속기관이 구독 중이 아닌 경우, 오후 4시부터 익일 오전 7시까지 원문보기가 가능합니다.

          무극 광화대는 인리형 분지인 백악기 음성분지와 단층 접촉하는 백악기 흑운모 화강암을 모암으로 하여 배태된 광상들로 구성되며, 광화대 북측에서 남측으로 무극${\cdot}$금왕${\cdot}$금봉 태극 광산의 순서로 배태된다. 맥의 산상, 광물학적, 유체포유불 및 등위원소 연구결과에 의하면, 북측 광화대의 무극광산은 상대적으로 높은 금-은비를 나타내는 전형적 복성맥의 구조를 보이며, 대체로 견운모화작용${\cdot}$녹니석화작용${\cdot}$녹염석화작용이 우세하게 관찰된다. 무극광산의 광화유체는 비교적 고온${\cdot}$고염도(=$300^{\circ}C$, 1~9 equiv. wt. % NaCl)와 물- 암석 상호반응이 진행된 광화유체($\delta^{18}O$; -1.2~3.7$\textperthousand$)로부터 냉각 및 희석작용의 진화양상을 보이며, 에렉트럼과 황화광물의 광물조합을 보이는 금광화기의 유황분압 및 정출온도는 $10^{-11.5}$~$10^{-13.5}$ atm과 267~$220^{\circ}C$를 보인다. 반면, 남측의 금왕${\cdot}$금봉${\cdot}$태극광산에서는 북측에 비해 낮은 금-은비를 보이는 단성맥 또는 망상세맥이 우세하게 산출되며, 캐올린화작용${\cdot}$규화삭용${\cdot}$탈산염화작용${\cdot}$스멕타이 트화작용이 광범위하게 분포하는 특징을 보인다. 이들 광산의 광화유체는 지표수의 다량 혼입에 의한 순환수 기원 ($\delta^{18}O$; -1.2~3.7$\textperthousand$)의 저온${\cdot}$저염 광화유체(<$230^{\circ}C$, <3 equiv. wt. % NaCl)로부터 $CO_2$ 비등 및 냉각작용에 의한 진화양상을 보인다. 황화광물과 에렉트림 이외에도 다양한 함은황염 광물이 우세하게 산출되는 이들 광산의 은광화기는 $10^{-15}$ ~$10^{-18}$ atm 과 200~15$0^{\circ}C$의 유황분압 및 정출온도를 보인다. 이들 연구결과는 무극광화대가 지표수의 다량 유입이 가능한 천부 지질환경임을 시사하며, 성 인적으로는 저유황형 천열수 광상으로 해석된다. 또한 광화대 북측과 남측에서의 광석광물, 이차변질광물 및 열수변질대의 분포, 광화유체 특성에 따른 전반적인 차이는 광화대내의 열적 중심부(무극광산)으로부터 열수계 최외각부(태극광산)가지의 열수계의 진화과정을 반영한 광산들의 시${\cdot}$공간적 분포에 기인한 것으로, 이는 열수계 진화과정시 유체간 혼합과정 및 광화유체 희석작용, 그리고 온도감소에 따른 금은광물 의 상이한 정출 환경에 기인한 것으로 해석된다. The gold-silver vein deposits in the Mugeug mineralized area are emplaced in late Cretaceous biotite granite associated with the pull-apart type Cretaceous Eumseong basin. Mugeug mine in northern part is composed of multiple veins showing relatively high gold fineness and is characterized by sericitization, chloritization and epidotization. The ore-forming fluids were evolved by dilution and cooling mechanisms at relatively high temperature and salinity (=30$0^{\circ}C$,1~9 equiv. wt. % NaCl) and highly-evolved meteoric water ($\delta$$^{18}$ O;-1.2~3.7$\textperthousand$) and gold mineralization associated with sulfides tormed at temperatures between 260 and 22$0^{\circ}C$ and within sulfur fugacity range of 10$^{-11.5}$ ~ 10$^{-13.5}$ atm. In contrast, Geumwang, Geumbong and Taegueg mines show the low fineness values, in southern part are characterized by increasing tendency of simple and/or stockwork veins and by kaolinitization, silicificatitan, carbonatization and smectitization. These droposits formed at relatively low temperature and salinity (<23$0^{\circ}C$, <3 equiv. wt. % NaCl) from ore-forming fluids containing greater amounts of less-evolved meteoric waters ($\delta$$^{18}$ O;-5.5~4.0$\textperthousand$), and silver mineralization representing various gold-and/or silver-bearing minerals formed at temperatures between 200 and 15$0^{\circ}C$ and from sulfur fugacity range of 10$^{-15}$ ~10$^{-18}$ atm These results imply that mineralization in the Mugueg area formed at shallow-crustal level and categorize these deposits as low-sulfidation epithermal type. The genetic differences between the northern and southern parts reflect the evolution of the hydrothermal system due to a different physicochemical environment from heat source area (Mugeug mine) to marginal area (Taegeum mine) in a geothermal field.

        • KCI등재

          한국 동남부지역 금·은 광상산 에렉트럼의 화학조성

          최선규,박맹언,최상훈,Choi,,Seon-Gyu,Park,,Maeng-Eon,Choi,,Sang-Hoon 대한자원환경지질학회 1994 자원환경지질 Vol.27 No.4

          Gold and/or silver mineralization in the southeast province, Korea, occurred in hydrothermal quartz vein that fills fracture zones in Cretaceous volcanic and sedimentary rocks of the Gyeongsang basin or granites and Precambrian gneiss. Most of the gold-silver-bearing veins in the province occur in Hapcheon, Suncheon and Haman-Gunbuk area where they are associated with Cretaceous Bulgugsa granites. On the basis of the Ag/Au ratio on amounts produced and ore grades, mode of occurrence, and associated mineral assemblages, hydrothermal Au-Ag deposits in southeast province, Korea, can be classified as follows: pyrite-type gold deposit (Group IIB, Samjeong and Sangchon deposits), antimony-type gold-silver deposit (Group IV, Gisan and Geochang deposits), and antimony-type silver deposit (Group V, Sanggo, Seweon, Seongju and Gahoe deposits). All of the gold-silver deposits in the province are generally characteristics of the gold-silver or silver-dominant type deposit which contains more silver-bearing minerals than those deposits in central Korea. The gold-silver mineralization in the deposits consist of two generation; the early characterized by gold precipitation and the late represented by silver-rich (as silver-bearing sulfosalts minerals) mineralization. All but one deposit (Samjeong deposit) having relatively lower Au content in electrum values between ${\approx}20$ and ${\approx}50$ atomic %. The mineralogical data on electrum-sphalerite and/or arsenopyrite geothermometry and fluid inclusion data indicate that the gold and silver mineralizations were occurred at temperatures of $190{\sim}280^{\circ}C$ and $150{\sim}180^{\circ}C$, respectively. These suggest that the gold-silver mineralization in the province occurred in the lower temperature and pressure conditions as epithermal-type hydrothermal vein deposit.

        • KCI등재

          한국 동남부지역 금은광산산 에렉트럼의 화학조성

          최선규,박맹언,최상훈 대한자원환경지질학회 1994 자원환경지질 Vol.27 No.4

          '스콜라' 이용 시 소속기관이 구독 중이 아닌 경우, 오후 4시부터 익일 오전 7시까지 원문보기가 가능합니다.

        맨 위로 스크롤 이동