dc.contributor | CNR | |
dc.contributor | Universidade Estadual de Campinas (UNICAMP) | |
dc.contributor | Univ Pavia | |
dc.contributor | Universidade Estadual Paulista (Unesp) | |
dc.contributor | Univ Nacl Salta | |
dc.date.accessioned | 2014-05-20T13:22:56Z | |
dc.date.available | 2014-05-20T13:22:56Z | |
dc.date.created | 2014-05-20T13:22:56Z | |
dc.date.issued | 2007-06-01 | |
dc.identifier | Geostandards and Geoanalytical Research. Malden: Wiley-blackwell, v. 31, n. 2, p. 105-124, 2007. | |
dc.identifier | 1639-4488 | |
dc.identifier | http://hdl.handle.net/11449/6828 | |
dc.identifier | 10.1111/j.1751-908X.2007.00844.x | |
dc.identifier | WOS:000247205300004 | |
dc.identifier | 1543738193935256 | |
dc.description.abstract | New analyses have been performed in order to enhance the data-set on the independent ages of four glasses that have been proposed as reference materials for fission-track dating. The results are as follows. Moldavite - repeated (40)Ar/(39)Ar age determinations on samples from deposits from Bohemia and Moravia yielded an average of 14.34 +/- 0.08 Ma. This datum agrees with other recent determinations and is significantly younger than the (40)Ar/(39)Ar age of 15.21 +/- 0.15 Ma determined in the early 1980s. Macusanite (Peru) -four K-Ar ages ranging from 5.44 +/- 0.06 to 5.72 +/- 0.12 Ma have been published previously. New (40)Ar/(39)Ar ages gave an average of 5.12 +/- 0.04 Ma. Plateau fission-track ages determined using the IRMM-540 certified glass and U and Th thin films for neutron fluence measurements agree better with these new (40)Ar/(39)Ar ages than the previously published ages. Roccastrada glass (Italy) - a new (40)Ar/(39)Ar age, 2.45 +/- 0.04 Ma, is consistent with previous determinations. The Quiron obsidian (Argentina) is a recently discovered glass that has been proposed as an additional reference material for its high spontaneous track density (around 100 000 cm(-2)). Defects that might produce spurious tracks are virtually absent. An independent (40)Ar/(39)Ar age of 8.77 +/- 0.09 Ma was determined and is recommended for this glass. We believe that these materials, which will be distributed upon request to fission-track groups, will be very useful for testing system calibrations and experimental procedures. | |
dc.language | eng | |
dc.publisher | Wiley-Blackwell | |
dc.relation | Geostandards and Geoanalytical Research | |
dc.relation | 3.929 | |
dc.relation | 1,430 | |
dc.rights | Acesso restrito | |
dc.source | Web of Science | |
dc.subject | fission-track dating | |
dc.subject | (40)Ar/(39)Ar dating | |
dc.subject | natural glasses | |
dc.subject | age standards | |
dc.title | New constraints on ages of glasses proposed as reference materials for fission-track dating | |
dc.type | Artículos de revistas | |