ケステル: トルコのタウロス山脈にある青銅器時代初期の亜鉛鉱石の源
Science (New York, N.Y.)
|April 14, 1989
まとめ
考古学者はトルコで古代の鉱山を発見し,銅器時代の金属生産に不可欠な亜鉛鉱石であるカシテライトを含んでいた. この発見は,青銅時代の亜鉛の潜在的源泉を提供し,地域経済の理解を複雑にしています.
科学分野:
- 考古学考古学とは
- 地質学 地質学 地質学
- 材料科学 材料科学とは
背景:
- 青銅器時代には青銅の生産のためにチンが必要でしたが,地質学的分布は稀です.
- 青銅時代の亜鉛の起源を理解することは,古代の経済と貿易ネットワークの再構築に不可欠です.
- 初期の金属交換におけるアナトリアの役割は,依然として活発な研究分野である.
研究 の 目的:
- トルコのケステル鉱山を調査し,古代の鉱業活動の証拠を探しました.
- ケステル遺跡に存在する鉱物資源を特定するために.
- 青銅時代のチンの潜在的源泉としてのケステル鉱山の重要性を評価する.
主な方法:
- 考古学的な発見の放射性炭素年代測定.
- 時系列的な評価のための陶器類型学.
- 鉱床 (カシテライト) を特定するための地質学的分析.
- 考古学的な発掘と調査.
主要な成果:
- ケステル鉱山は紀元前3千年に遡る.
- カシテライト (亜鉛酸化物) は,鉱山の破片や近くの地質学的形成物で特定されました.
- この鉱山は,重要な古代の亜鉛鉱石の源である.
結論:
- ケステル鉱山は重要な発見であり,青銅時代の亜鉛の源泉を提供している.
- この発見は,青銅時代のアナトリアにおける地域経済パターンの既存のモデルに挑戦しています.
- この発見は,都市化の初期に東地中海における地域間の金属交換を再評価することを必要としている.
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