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Explore Regional Characteristics and Design to Enhance New Elements of Brand Packaging--Taking Moutai as an Example
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作者 Zongshe Kang Dahlan Bin Abdul Ghani 《Journal of Sustainable Business and Economics》 2024年第2期62-68,共7页
Taking ethnic minority culture as the starting point,this paper explores the possibility of artistic expression of elements in different regions,and explores how regional brands can combine regional culture to create ... Taking ethnic minority culture as the starting point,this paper explores the possibility of artistic expression of elements in different regions,and explores how regional brands can combine regional culture to create market effects and public preferences.Through field research,literature research,and market case comparison,the aesthetic symbols of different cultural and artistic forms of the Dong ethnic group are refined and expressed,and their application in the development of local brand design is explored.Artistic expression elements such as patterns,colors,and materials are extracted from the architectural culture,ethnic art,and daily food customs of the Dong ethnic group,and used in the design of regional wine products,deeply connecting regional culture and regional brands.In the design,we should pay attention to national characteristics and brand effects,and carry out the design from a multi-dimensional design perspective,which will help to enhance brand competitiveness and achieve a win-win situation under the long-term goal of promoting national self-confidence and inheriting the essence of national culture. 展开更多
关键词 Moutai liquor dongsu brand Characteristic design Competitiveness enhancement
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内蒙古苏尼特左旗东苏A型花岗岩的锆石U-Pb年龄、地球化学特征及地质意义 被引量:10
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作者 俞礽安 胡鹏 +4 位作者 曾威 李志丹 刘晓雪 张超 郭虎 《岩石矿物学杂志》 CAS CSCD 北大核心 2016年第2期229-241,共13页
位于苏尼特左旗东部的东苏二长花岗岩是索伦缝合带重要组成部分,具有高硅(SiO_2=69.76%~75.58%)、高碱且相对富钾(K2O+Na2O=6.99%~9.16%,K2O/Na2O=0.70~1.69)、相对富铝(铝饱和指数A/CNK=1.04~1.13)、高TFeO/MgO值(3.43~11... 位于苏尼特左旗东部的东苏二长花岗岩是索伦缝合带重要组成部分,具有高硅(SiO_2=69.76%~75.58%)、高碱且相对富钾(K2O+Na2O=6.99%~9.16%,K2O/Na2O=0.70~1.69)、相对富铝(铝饱和指数A/CNK=1.04~1.13)、高TFeO/MgO值(3.43~11.26)、贫镁(MgO=0.08%~0.50%)的特征;微量元素地球化学性质表现出相对富集轻稀土,Ba、Sr、Nb、Eu强烈负异常,Rb、Th、Ta等不相容元素富集的特征。主量和微量元素均表现出铝质A型花岗岩的特征。采用锆石LA-ICP-MS U-Pb法获得206Pb/238U值的加权平均年龄为221.5±0.81 Ma(MSDN值为0.57),表明该岩体为晚三叠世岩浆活动的产物。结合区域地质资料及地球化学信息可以判断该东苏花岗岩为后造山伸展阶段长英质地壳物质(变杂砂岩)部分熔融的产物。它的出现,标志着古亚洲洋演化的结束,索伦缝合带在晚三叠世的碰撞已达末期。 展开更多
关键词 A型花岗岩 后造山伸展 晚三叠世 索伦缝合带 东苏岩体
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