半干旱的中哈萨克斯坦塞米兹布古地表遗址综合体的石器物风化特征
Emily Coco1,2, Patrick Schimdt3,4, Bin Hu5
1Center for the Study of Human Origins, Department of Anthropology, New York University, 25 Waverly Place, New York, NY 10009, USA.
概括
在Semizbugu的考古岩石风化阶段进行了分析. 表面粗度降低和孔隙增加可能为石器提供相对的时间顺序,但漆颜色不可靠.
科学领域:
- 考古学
- 地质科学
- 材料科学
背景情况:
- 岩石表面的气候变化对于考古时间表,气候研究和文物认证至关重要.
- 由于多因素的形成过程,了解石器上的岩层是复杂的.
- 之前的研究已经使用了气候变化阶段来分类文物, 但根本的过程尚未完全理解.
研究的目的:
- 调查石材涂层形态的差异,元素组成,以及在Semizbugu的气候阶段的表面粗度.
- 识别在半干旱环境中导致文物气候变化的过程.
- 开发一种更可靠的石器手工艺品时间排序方法.
主要方法:
- 分析岩石涂层形态,元素组成和石器工件的表面粗性.
- 对气候变化的宏观识别.
- 在单一原料类型内对气候变化的比较.
主要成果:
- 在Semizbugu发现多种气候变化过程,包括风磨损和表面溶解.
- 一个潜在的时间模型,基于表面粗度的降低和表面孔隙的增加.
- 由于磨损和形成不规则,石漆颜色在时间评估中被认为不可靠.
结论:
- 在Semizbugu的文物可以通过评估表面粗和坑洞来相对顺序排列.
- 在这种半干旱的环境中,不应使用岩石漆颜色进行时间评估.
- 建议通过光学刺激发光 (OSL) 来测定岩层暴露时间,以验证时间模型和理解文物回收事件.
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