从颜料的物理化学分析看秘鲁南部的岩画

IF 0.9 4区 艺术学 0 ARCHAEOLOGY Rock Art Research Pub Date : 2024-01-29 DOI:10.56801/rar.v41i1.276
Józef Szykulski, Beata Miazga, J. Wanot
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引用次数: 0

摘要

本文介绍了一支国际考古探险队于 2017 年和 2019 年在秘鲁南部卡普利纳河流域的 Río Atico 盆地和 Vilavilani 地区的众多隐蔽遗址进行研究期间记录的岩画。研究期间,对岩画考古遗址进行了登记,记录了岩画的保存状况,并确定了造成岩画破坏/退化的因素。此外,还确定了岩画的形式和主题范围,同时界定了该地区岩画的四种风格/造型惯例(风格 1-4)。对表现形式/绘画的叠加进行了新的安排,从而有可能确定其创作的时间顺序(相对年代学)。还对着色物质进行了多方面的物理化学分析,从而确定了它们的化学成分。所有着色物质的矿物来源都得到了证实,即它们应被描述为无机颜料。同时,还得出了关于用于获取这些物质的原材料来源的结论。在研究过程中,观察到个别绘画作品的颜色发生了变化,这为得出导致这些变化的化学过程的结论提供了依据。
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ROCK PAINTING WITHIN SOUTHERN PERU IN THE CONTEXT OF PHYSICOCHEMICAL ANALYSIS OF PIGMENTS
The article pertains to rock paintings recorded during studies conducted in 2017 and 2019 by an international archaeological expedition at numerous sheltered sites in the Río Atico basin and Vilavilani region in the Río Caplina catchment area within southern Peru. During the research, archaeological sites with rock art were registered, the state of preservation of the paintings was documented, and it was determined what factors were causing their destruction/degradation. The form and thematic scope of the paintings were also determined while defining four styles/stylistic conventions (styles 1–4) of the rock painting in the area in question. New arrangements regarding the superposition of representations/paintings made it possible to define the time sequence of their creation (relative chronology). Multifaceted physicochemical analyses of colouring substances were also carried out, which allowed determining their chemical composition. The mineral origin of all colouring substances has been confirmed, i.e. they should be described as inorganic pigments. At the same time, conclusions regarding the source of origin of the raw material used for their acquisition were presented. During the research, changes in the colours of individual paintings were observed, which provides the basis for conclusions regarding the chemical processes that caused them.
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Rock Art Research
Rock Art Research Multiple-
CiteScore
1.80
自引率
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