2009
DOI: 10.1007/s12520-009-0010-7
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Combined Pb–Sr isotopic analysis in provenancing late Roman iron raw materials in the territory of Sagalassos (SW Turkey)

Abstract: In early Roman times, iron was likely supplied to the city of Sagalassos through the smelting of close-by hematite ores. In the early Byzantine period, magnetitetitanite placer sands in some instances could have been exploited for its iron. For the intermediate late Roman period, however, the source of the locally used iron was unknown. Pb and Sr isotopic analyses of iron ores from the area of Camoluk, just south of the territory of Sagalassos, and of late Roman iron artefacts from the antique city itself, rev… Show more

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Cited by 15 publications
(18 citation statements)
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“…Debate, too, has been limited, resulting in multiple analytical strategies and few opportunities for demonstrating their general applicability. Among the approaches taken are chemical analyses of the metal in comparison to potential ores (Devos et al, 2000), isotopic ratio analysis of the metal in comparison to potential ores (Degryse et al, 2007(Degryse et al, , 2009Schwab et al, 2006) and, most commonly, the chemical analysis of slag inclusions (SIs) in the metal in comparison to potential ironmaking regions or ore bodies (Blakelock et al, 2009;Buchwald, 2005;Coustures et al, 2003Coustures et al, , 2006Desaulty et al, 2008;Desaulty et al, 2009;Gordon and van der Merwe, 1984;Hedges and Salter, 1979;Leroy, 2010, Leroy et al, 2011, 2012.…”
Section: Introductionmentioning
confidence: 99%
“…Debate, too, has been limited, resulting in multiple analytical strategies and few opportunities for demonstrating their general applicability. Among the approaches taken are chemical analyses of the metal in comparison to potential ores (Devos et al, 2000), isotopic ratio analysis of the metal in comparison to potential ores (Degryse et al, 2007(Degryse et al, , 2009Schwab et al, 2006) and, most commonly, the chemical analysis of slag inclusions (SIs) in the metal in comparison to potential ironmaking regions or ore bodies (Blakelock et al, 2009;Buchwald, 2005;Coustures et al, 2003Coustures et al, , 2006Desaulty et al, 2008;Desaulty et al, 2009;Gordon and van der Merwe, 1984;Hedges and Salter, 1979;Leroy, 2010, Leroy et al, 2011, 2012.…”
Section: Introductionmentioning
confidence: 99%
“…We know that these minerals were mined on a fairly large scale (Salazar et al 2011;Salinas and Salazar 2008;Vaughn et al , 2013), yet, little archaeometric research has focused on characterizing iron oxides. This is quite unlike the growing archaeometric literature on iron oxides in other regions (e.g., Erlandson et al 1999;Degryse et al 2009;Kiehn et al 2007;Mooney et al 2003;Popelka-Filcoff et al 2007, 2008Smith and Pell 1997;Weinstein-Evron and Ilani 1994).…”
Section: Introductionmentioning
confidence: 63%
“…These reference materials were selected because they have known isotopic compositions and contain approximately 300–500 μg g −1 Sr and/or Pb, which is comparable to values found in archaeological glasses (Degryse et al . ). For Sr isotopic determination, reference materials with Rb/Sr ratios below 0.2 were selected.…”
Section: Methodsmentioning
confidence: 97%
“…Reference materials included NIST SRM 610 (National Institute for Standards and Technology, Gaithersburg, MD, USA) and USGS reference materials BHVO-2G, NKT-G and GSE-1G (United States Geological Survey, Reston, Virginia, USA). These reference materials were selected because they have known isotopic compositions and contain approximately 300-500 lg g -1 Sr and/or Pb, which is comparable to values found in archaeological glasses (Degryse et al 2009). For Sr isotopic determination, reference materials with Rb/Sr ratios below 0.2 were selected.…”
Section: Reagents Samples and Reference Materialsmentioning
confidence: 99%