2019
DOI: 10.1007/s12520-019-00782-y
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Rock-magnetic and color characteristics of archaeological samples from burnt clay from destructions and ceramics in relation to their firing temperature

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Cited by 22 publications
(11 citation statements)
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“…Finally, the NRM of the samples was thermally demagnetized with a TD-48 SC (ASC Scientific) furnace in several steps of 20 or 40 o C, up to a maximum temperature varying from 560 to 640 o C at which all samples were completely demagnetized. After each heating-cooling step, the bulk magnetic susceptibility at room temperature was measured to detect possible magnetic mineralogy changes occurred during the laboratory heating and to obtain information about the equivalent maximum firing temperatures of the rings (Rasmussen et al 2012;Jordanova et al 2019).…”
Section: Methodsmentioning
confidence: 99%
“…Finally, the NRM of the samples was thermally demagnetized with a TD-48 SC (ASC Scientific) furnace in several steps of 20 or 40 o C, up to a maximum temperature varying from 560 to 640 o C at which all samples were completely demagnetized. After each heating-cooling step, the bulk magnetic susceptibility at room temperature was measured to detect possible magnetic mineralogy changes occurred during the laboratory heating and to obtain information about the equivalent maximum firing temperatures of the rings (Rasmussen et al 2012;Jordanova et al 2019).…”
Section: Methodsmentioning
confidence: 99%
“…Archaeologically, magnetic analysis has been utilized to understand the formation and preservation of a combustion event, which normally produce very fine-grained particles as well as maybe haematite and/or magnetite depending on the atmosphere and prevailing combustion conditions (oxidizing vs. reducing), among other factors. It has further been used to explore postdepositional disturbances that may enhance or remove such particles from a deposit (Bradák et al, 2020;Carrancho & Villalaín, 2011;Carrancho et al, 2009;Dearing, 1999;Dearing et al, 1996b;Herries, 2006;Jordanova et al, 2019). (Marean et al, 2007), stone tool heat treatment (Brown et al, 2009), microlithic technology (Brown et al, 2009(Brown et al, , 2012 and the influence of the Toba supervolcano on African hunter-gatherers (Smith et al, 2018).…”
Section: Background To Magnetic Analysismentioning
confidence: 99%
“…Factors that enhance the anthropogenic magnetic signature include the source of the burnt sediment, with greater enhancement occurring in deposits derived from magnetically weaker rock strata, as well as the temperature of combustion along with the longevity of the process. Furthermore, the amount of oxygen and organic material available while heating will also have an effect (Herrejón Lagunilla et al, 2019; Herries, 2006; Herries & Fisher, 2010; Jordanova et al, 2019). The frequency of repeated burnings will further influence the degree of enhancement and influence the signature (Herries & Fisher, 2010; Herries & Latham, 2009).…”
Section: Introductionmentioning
confidence: 99%
“…According to Kreimeyer (1987) and Anwar et al (2011), red tones become weaker when more iron is incorporated into the structure of the compounds and less remains in the iron oxides. Mention by (Jordanova, 2019) Iron oxides, especially magnetite (Fe3O4) and hematite (α-Fe2O3) are the key minerals for tracking the thermal transformations undergone by burnt clay materials. As with this study, the first step is to test the raw materials to identify their mineral composition and conduct research on the suitability of mixing terracotta with glaze materials (simple additions to base glaze), including a view on fluxes and the percentage of terracotta to mix with colors for the glaze.…”
Section: Introductionmentioning
confidence: 99%