Isotopic Analysis 2012
DOI: 10.1002/9783527650484.ch13
|View full text |Cite
|
Sign up to set email alerts
|

Archeometric Applications

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

0
6
0

Year Published

2015
2015
2024
2024

Publication Types

Select...
4
2

Relationship

0
6

Authors

Journals

citations
Cited by 7 publications
(6 citation statements)
references
References 99 publications
0
6
0
Order By: Relevance
“…Several studies have been reported in the literature. 37,52,76–80 Here, three different methods are detailed. The first derives the error multiplication factor ( F ) as a function of the mixture isotope ratio, leading to a very simple formula to derive the optimal isotope ratio for the mixture.…”
Section: Implementing Isotope Dilutionmentioning
confidence: 99%
See 2 more Smart Citations
“…Several studies have been reported in the literature. 37,52,76–80 Here, three different methods are detailed. The first derives the error multiplication factor ( F ) as a function of the mixture isotope ratio, leading to a very simple formula to derive the optimal isotope ratio for the mixture.…”
Section: Implementing Isotope Dilutionmentioning
confidence: 99%
“…This method calculates the F factor as a function of the ratio between the amount of sample and the amount of spike. 52 It is essentially eqn (15), rewritten, by introducing α ( n S / n T atomic ratio) into eqn (1), which leads to eqn (19)…”
Section: Implementing Isotope Dilutionmentioning
confidence: 99%
See 1 more Smart Citation
“…Extremely careful sample purication is usually a key point of such research but it is effective for relatively large samples (>100 mg) with relatively high lead levels (range of &). However, in most research on historic objects or works of art, 13,[15][16][17][18][19][20] the availability of such samples is rare. Commonly, the sample quantities that can be used for analysis, especially archaeological artefacts, inks or pigments are extremely low.…”
Section: Introductionmentioning
confidence: 99%
“…However, it is well-established that anthropic activities have modified the natural seawater lead isotopic signature and isotopic analyses have long been employed to identify the source of lead present in the marine environment [13][14][15][16][17]. Lead isotopes are also used as a tracer in archaeological science, where they allow tracing of the origin of artifacts by relating them to their geological raw material [18][19][20][21][22]. The recent application of isotopic analysis to archaeological ceramics from multiple contexts in the Eastern Mediterranean and Ancient Mexico, demonstrates that lead isotopes constitute a powerful analytical tool to both discriminate between ceramics of different origins and to relate ceramics to their source, either by comparison with ceramics of known origin or their raw materials [23,24].…”
Section: Introductionmentioning
confidence: 99%