埃塞俄比亚的黑曜石:地质考古学的观点

A. Negash
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引用次数: 0

摘要

在埃塞俄比亚,黑曜石主要产于阿法尔坳陷和埃塞俄比亚主裂谷。这些黑曜岩的组成和岩石学特征各不相同。一些火山中心表明,来自单一中心的不同火山喷发不一定意味着不同的化学性质。使用K/Ar、Ar/Ar和裂变径迹法测定了黑曜石的年代,以确定喷发的时间,但也有一些通过水合作用测年的人工制品的日期,以确定工具制造的时间。至少从早期石器时代开始,许多地质资源就被史前人口利用,但黑曜石在石器时代中期开始普遍使用。黑曜石为基础的石器工具在埃塞俄比亚一直使用到最近。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Obsidian in Ethiopia: a Geoarchaeological perspective
In Ethiopia, obsidian is mainly found in the Afar Depression and the Main Ethiopian Rift. The compositional and petrological features of these obsidians vary. Some volcanic centers show that varying volcanic eruptions from a single center may not necessarily imply variable chemistry. Obsidian has been dated using K/Ar, Ar/Ar, and fission track methods to determine the time of eruption but there are also a few dates on artifacts by hydration dating to establish the time of tool manufacture. Many of the geological sources were utilized by prehistoric populations beginning at least since the Early Stone Age but obsidian became commonly used during the Middle Stone Age. Obsidian based stone tool use for scraping in Ethiopia persisted until recent times.
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