• (The) Research of the performance art and culture
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• no.33
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• pp.129-163
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• 2016

This study examines processes of cultural introductions and transformations among Korea, China and Japan via focuses on the formative characteristics of nasori(納曾利) masks belonging to komagaku (高麗樂), part of bugaku (舞樂), a Japanese court dance and music. Previous studies of traditional masks in East Asia focus on their dramatic characters and entertaining aspects. On the contrary, it approaches to their origins through the formative characteristics of komagaku nasori masks. Prince of Lanling, the representative togaku passed to Japan, and komagaku nasori perform a pair of toubu (答舞). One formative characteristic between Prince of Lanling and nasori masks is a dangling jaw (吊り顎). Masks having 'he' (へ)-shaped eyes like Japan's okina (翁) masks are characterized by a division (切顎) between the face and jaw, which is as same as the Korean masks. Other common grounds between Prince of Lanling and nasori masks are grotesque ghost faces and concentric double-circled eyes with their outlines painted gold. Concentric double-circled eyes prove that they spread to broader areas before the age of togaku and developed into a variety of divine-animal mask patterns. That Korean masks and nasori masks both have concentric double-circled eyes and dangling jaws is a significant starting point in studying the origin of traditional performing art in East Asia. Japan's bugaku has been passed down in shrines as part of folk religion. However, there exist in Korea no records or examples related to komagaku nasori masks introduced to Japan. This study provides some clues to comparison between Korean masks and komagaku nasori masks by focusing on the formative characteristics of the latter. The researcher suggests a new perspective to nasori mask dance by re-examining earlier Korean studies of the introduction of Daemyeonmu of Prince of Lanling to Japan through Shilla and the assumption of Nasori as Shilla music.

• The Journal of Engineering Geology
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• v.32 no.4
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• pp.611-625
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• 2022

One of the applications of geomagnetic paleo-secular variation (PSV) is the age dating of archeological remains (i.e., the archeomagnetic dating technique). This application requires the local model of PSV that reflects non-dipole fields with regional differences. Until now, the tentative Korean paleosecular variation (t-KPSV) calculated based on JPSV (SW Japanese PSV) has been applied as a reference curve for individual archeomagnetic directions in Korea. However, it is less reliable due to regional differences in the non-dipole magnetic field. Here, we present PSV curves for AD 1 to 600, corresponding to the Korean Three Kingdoms (including the Proto Three Kingdoms) Period, using the results of archeomagnetic studies in the Korean Peninsula and published research data. Then we compare our PSV with the global geomagnetic prediction model and t-KPSV. A total of 49 reliable archeomagnetic directional data from 16 regions were compiled for our PSV. In detail, each data showed statistical consistency (N > 6, 𝛼₉₅ < 7.8°, and k > 57.8) and had radiocarbon or archeological ages in the range of AD 1 to 600 years with less than ±200 years error range. The compiled PSV for the initial six centuries (KPSV0.6k) showed declination and inclination in the range of 341.7° to 20.1° and 43.5° to 60.3°, respectively. Compared to the t-KPSV, our curve revealed different variation patterns both in declination and inclination. On the other hand, KPSV0.6k and global geomagnetic prediction models (ARCH3K.1, CALS3K.4, and SED3K.1) revealed consistent variation trends during the first six centennials. In particular, the ARCH3K.1 showed the best fitting with our KPSV0.6k. These results indicate that contribution of the non-dipole field to Korea and Japan is quite different, despite their geographical proximity. Moreover, the compilation of archeomagnetic data from the Korea territory is essential to build a reliable PSV curve for an age dating tool. Lastly, we double-check the reliability of our KPSV0.6k by showing a good fitting of newly acquired age-controlled archeomagnetic data on our curve.