• Title/Summary/Keyword: 무생

Search Result 2, Processing Time 0.015 seconds

A Study of Sheng's Stage Costume in Peking Opera (경극에 표현된 “생”의 무대의상 연구)

  • 이영숙
    • The Research Journal of the Costume Culture
    • /
    • v.12 no.4
    • /
    • pp.599-613
    • /
    • 2004
  • The purpose for this paper is to find the common characteristics of Korean traditional clothing, which is largely affected by Chinese arts and culture. There are many different theories about Faking Opera's orgine but an established character is an ensemble song and dance. It virtually represent overall Chinese arts. There are four characters in the Peking Opera ; Sheng, Dan, Jing, and Chuck. Sheng is divided into Nosheng, Sosheng, Musheng and Hongsheng based on their dramatic skills. Also, Sheng requires various acting skills : song, dance, dialogue, act and fighting skill. Peking Opera's stage costume was set up in Qing dynasty though it's style was embellished with mainly Ming dynasty's clothing style. The rankings and personalties of the role are strictly applied to decide what to wear. Artistic exaggeration, symbol and transfiguration, use of colors are equally important in planning the stage costume.

  • PDF

Paleoenvironments in Western Part of the East Sea, Korea, during the Late Quaternary Using Benthic Foraminifera (저서성 유공충에 의한 한국 동해 서부 해역의 제 4기 후반 고해양환경 연구)

  • 우한준;정혜경
    • 한국해양학회지
    • /
    • v.30 no.5
    • /
    • pp.493-511
    • /
    • 1995
  • Analysis of the Late Quaternary benthic foraminifera in the cores from the western part of the East Sea, Korea, indicates several distinct changes in the paleoenvironments during the deposition. The palecology of biofacies of Cores PC-1 from the upper slop and PC-2 from the rise shows several distinct changes in bottom water temperatures during the late Quaternary. The Core PC-4 from the Ulleung Basin generally consists of agglutinated genus, Muiliammina, and anaerobic calcareous genus, Bolivina, in biofacies, suggesting that the anoxic bottom condition was prevailed during the deposition. Benthic foraminiferal rare or barren zones in the Cores indicate the limits of water circulation caused by lower sea-level in the regions during the glacial period through the Late Quaternary. The changes of benthic foraminiferal biofacies reflect temporal and spacial variations in overall bottom environments, such as bottom water temperature, dissolved oxygen, and water circulation pattern. The benthic foraminiferal data can be used to interpret paleoclimatic conditions and predict global sea-level changes, and the results of these studies should be useful to understand the evolutional history of the East Sea through the Late Quaternary.

  • PDF