Identification of “red ochre‿in soil at Kfar HaHoresh Neolithic site, Israel: Magnetic measurements coupled with materials characterization
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- 作者：Alexander Tsatskina ; tsatskin@research.haifa.ac.il" class="auth_mail" title="E-mail the corresponding author ; Tatyana S. Gendlerb ; 1
- 关键词：Fired clay ; Fe(III)-smectite ; Terra Rossa ; Micromorphology ; Soil magnetism ; Early Neolithic
- 刊名：Journal of Archaeological Science: Reports
- 出版年：2016
- 出版时间：April 2016
- 年：2016
- 卷：6
- 期：Complete
- 页码：284-292
- 全文大小：1936 K
文摘
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Rock magnetism is applied to PPNB baked clay in Terra Rossa on Kfar HaHoresh site.
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In contrast to soil, baked clay has enhanced χLF, Js alongside lessened χFD and Bc.
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Mainly SD particles of hematite-magnetite formed during clay firing in air at ca. 800–850 °C
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Fe(III)-clay as a likely raw material underwent structural alterations on heating.
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Results provide evidence of sintered clay technology in Levant prior to ceramic Neolithic.