• Journal of Fashion Business
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• v.22 no.1
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• pp.82-99
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• 2018

The purpose of this study is to examine the characteristics that appeared in the fashion and colors of exotic tastes used by Renoir with a view to re-evaluating his-attitude towards exotic tastes. The methods used in this study were literature research and analysis of visual data from Renoir's works. The results of the study are as follows. Renoir's exotic tastes originated from the material perspective appearing in the fashions and accessories of Algeria, Orient, Spain, and Japan. Parisienne Odalisque Lise in Harem-style, Jeanne Samari in parisienne fashion holding a Japanese fan, and Gabriel in oriental fashion were portrayed as major muses. The Algerian style consisted of white, yellow or red veils, thobes, loose pants worn in Haik, and burnous. The Oriental-style was composed of harem pants, turbans, hair accessories, ornate zouave jackets, and oriental ornaments. The Spanish-style showed gay ornaments, fitted red or yellow matador costume, red bandannas, black hats, and red dresses, plus Spanish guitars. The Japanese-style consisted of kimonos, accessories such as fans, and backgrounds with interior articles such as vases, wall picture frames, and folding screens. The exotic fashion colors were red, yellow and white. Renoir expressed the works with his delicate skills and sense of craftsmanship, and he even added creative design portrayals sometimes. He selected fashions and accessories of exotic tastes as objects and expressed the objects with materials and colors reflecting regional characteristics as such, he can be regarded as an artist wed to who fashions of exotic tastes.

• Economic and Environmental Geology
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• v.52 no.3
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• pp.251-258
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• 2019

During the detailed geological survey around the southern Yangsan Fault, we newly found a Quaternary fault outcrop, which cuts unconsolidated sediments. The fault named the Sinwoo site, located in the Sinwoo pasture, Miho-ri, Duseo-myeon, Ulsan metropolitan city, is the first discovered Quaternary fault near the western part of the south Yangsan Fault. In this study, we provide information on characteristics of fault geometry and unconsolidated sediment at Sinwoo site based on the analysis data of topography, drainage, and lineament around the study site. The fault site is situated at pediment slope, but fan-shaped middle terrace, as well as thick sediment exposed at low terrace, indicates that the unconsolidated sediments have been deposited in the alluvial fan environment. The drainage develops to the third-order drainage system, and the first and the second drainage system meet at right angles to each other and form a radial drainage pattern. In addition, the NE-SW direction lineaments can be identified on the basis of the curvature of the river and the step of the topographic relief, running over the Sinwoo site. The fault of $N30-35^{\circ}E/79-82^{\circ}SE$ shows ~ 5.8 m apparent vertical offset and dominantly reverse-slip sense based on slickenline, rotation of pebbles, and drag folding at footwall. However, some discontinuous sediments observed in the footwall are interpreted as fissure-filling materials due to the strike-slip movement. Now, we are under multidisciplinary investigations of additional field survey and age dating in order to determine the evolution of Sinwoo site fault during the Quaternary.