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Mattinson, James M. (2005) Zircon U–Pb chemical abrasion (“CA-TIMS”) method: Combined annealing and multi-step partial dissolution analysis for improved precision and accuracy of zircon ages. Chemical Geology, 220 (1) 47-66 doi:10.1016/j.chemgeo.2005.03.011

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Reference TypeJournal (article/letter/editorial)
TitleZircon U–Pb chemical abrasion (“CA-TIMS”) method: Combined annealing and multi-step partial dissolution analysis for improved precision and accuracy of zircon ages
JournalChemical Geology
AuthorsMattinson, James M.Author
Year2005 (July)Volume220
Page(s)47-66Issue1
PublisherElsevier BV
DOIdoi:10.1016/j.chemgeo.2005.03.011Search in ResearchGate
Mindat Ref. ID294111Long-form Identifiermindat:1:5:294111:4
GUIDf92ae95b-406a-4e84-8032-b60ae863ad60
Full ReferenceMattinson, James M. (2005) Zircon U–Pb chemical abrasion (“CA-TIMS”) method: Combined annealing and multi-step partial dissolution analysis for improved precision and accuracy of zircon ages. Chemical Geology, 220 (1) 47-66 doi:10.1016/j.chemgeo.2005.03.011
Plain TextMattinson, James M. (2005) Zircon U–Pb chemical abrasion (“CA-TIMS”) method: Combined annealing and multi-step partial dissolution analysis for improved precision and accuracy of zircon ages. Chemical Geology, 220 (1) 47-66 doi:10.1016/j.chemgeo.2005.03.011
In(2005, July) Chemical Geology Vol. 220 (1) Elsevier BV

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

Bowring (1998) GSA Today A new look at evolutionary rates in deep time: uniting paleontology and high-precision geochronology 8, 1
Krogh (1974) Carnegie Inst. Yearbook Alteration in zircons with discordant U–Pb ages 73, 560
Krogh (1975) Carnegie Inst. Yearbook Alteration in zircons and differential dissolution of altered and metamict zircon 74, 619
Ludwig, K.R., 2000b. Isoplot/Ex 2.45, a geochronological toolkit for Microsoft Excel: Berkeley Geochronology Center.
Mattinson, J.M., 1997. Analysis of zircon by multi-step partial dissolutions: the good, the bad, and the ugly. GAC/MAC Ottawa '97 Abst. Vol., A98.
Mattinson (2000) Low-temperature U–Pb discordance mechanisms in zircons: the role of radiation damage and fluids vol. 81 (48)
Mattinson (2000) Suppl. Eos, Trans.-Am. Geophys. Union U–Pb zircon analysis by “chemical abrasion”: combined high-temperature annealing and partial dissolution analysis 8, S27
Mattinson (2003) CA (chemical abrasion)-TIMS: high-resolution U–Pb zircon geochronology combining high-temperature annealing of radiation damage and multi-step partial dissolution analysis vol. 84 (46)
Mattinson (1996) U–Pb reverse discordance in zircons: the role of fine-scale oscillatory zoning and sub-micron transport of Pb vol. 95, 355
Mortensen (1992) Evidence for high levels of unsupported radiogenic 207 Pb in zircon from a granitic pegmatite: implications for interpretation of discordant U–Pb data , 370
Mortensen (1997) Ion microprobe and cathodoluminescence investigations of unsupported 207 Pb in zircon , A105
Parrish (2003) Zircon U–Th–Pb geochronology by isotope dilution–thermal ionization mass spectrometry (ID-TIMS) 53, 183


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