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Age determination of travertine from archaeologic...
Journal article

Age determination of travertine from archaeologic sites

Abstract

Where travertine has formed by slow passage of calcite saturated water on to archaeological sites, the deposits of cultural materials may be enclosed within material which is datable by a number of isotopic methods. Th-230/U-234 dating is generally applicable for travertines which are not contaminated by detritus, not too porous or permeable, and containing more than 0.1 ppm of uranium. Travertines containing 1 ppm U or more can be also dated …

Authors

Schwarcz MP

Journal

Revue d Archéométrie, Vol. 4, No. 1, pp. 101–109

Publisher

PERSEE Program

Publication Date

1980

DOI

10.3406/arsci.1980.1116

ISSN

0399-1237