| | ICP-MS/TIMS ANALYSES OF MONAZITES AND XENOTIME FROM MIGMATITES IN THE AAR MASSIF (Site not responding. Last check: 2007-10-21) |
 | | Isotope dilution U-Th-Pb age determinations using a 205Pb/235U spike, and no chemical separation, were made on two 10-30 mg monazite grains and one xenotime grain from a sample of migmatites in the Aar Massif, Swiss Alps. |
 | | The xenotime grain yielded discordant results: 222 ± 14 Ma, 341 ± 14 Ma and 2890 ± 90 Ma, probably indicating its Alpidic formation with radiogenic Pb inherited from Precambrian zircon, and incorporation of additional Th. |
 | | As the xenotime analysis did not show this effect (and no-chemistry zircon single grain Pb analyses don’t either) the effect may be due to abundant Ce on the filament: Ce could act as an electron donor preventing the formation of Pb+. |
| gsa.confex.com /gsa/2002AM/finalprogram/abstract_45197.htm (548 words) |