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Greek Marbles

Determination of Provenance by Isotopic Analysis

Bibliographic Data

ID23321920
AuthorsHarmon Craig (Scripps Institution of Oceanography, University of California at San Diego, La Jolla 92037), Valerie Craig (Scripps Institution of Oceanography, University of California at San Diego, La Jolla 92037)
Year1972
Volume176
Issue4033
Pages401-403
Publication date1972-04-28
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueScience (JOURNAL)
Journal identifiersISSN: 0036-8075 • E-ISSN: 0193-4511
PublisherAmerican Association for the Advancement of Science (AAAS) (PUBLISHER)
DOI10.1126/science.176.4033.401
PMID17777722
OpenAlexW2074239818
LanguageEN
Citations received57
References cited6

A study has been made of carbon-13 and oxygen-18 variations in Greek marbles from the ancient quarry localities of Naxos, Paros, Mount Hymettus, and Mount Pentelikon. Parian, Hymettian, and Pentelic marbles can be clearly distinguished by the isotopic relationships; Naxian marbles fall into two groups characterized by different oxygen-18/oxygen-16 ratios. Ten archeological samples were also analyzed; the isotopic data indicate that the "Theseion" is made of Pentelic marble and a block in the Treasury of Siphnos at Delphi is probably Parian marble.

Archaeology · Geochemistry · Geography · Isotopes of oxygen · Mineralogy · Mount · Provenance · Archaeology and ancient environmental studies · Building materials and conservation · Geology · Maritime and Coastal Archaeology

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Unique citing works57
Citations per year1,08
Citation span1973 - 2026 (54)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 53

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