TY - JOUR
T1 - Understanding geologic processes with xenotime
T2 - Composition, chronology, and a protocol for electron probe microanalysis
AU - Hetherington, Callum J.
AU - Jercinovic, Michael J.
AU - Williams, Michael L.
AU - Mahan, Kevin
N1 - Funding Information:
Bartosz Budzyn, Peter Dahl, Christopher Daniel, Brian Wernicke and Maja Stanislawska are thanked for providing samples and images of xenotime for Figs. 2 and 6 . Matthew Horstwood, Frank Mazdab, Christopher McFarlane and Joe Pyle are also thanked for sharing their thoughts on the occurrence and analysis of xenotime. Two anonymous reviewers and the editorial support of Fritz Finger are also appreciated. This research was partly supported by National Science Foundation Grant EAR-0004077 to Williams and Jercinovic for development of the Ultrachron electron microprobe.
PY - 2008/9/15
Y1 - 2008/9/15
N2 - Xenotime (YPO4) is iso-structural with zircon-group minerals and lies at one end of a compositional solid-solution with monazite. As with monazite and zircon, naturally occurring xenotime may accommodate significant concentrations of rare earth elements, as well as Th and U, making it an important repository for these valuable geochemical marker elements and a potential geochronometer. Xenotime grows in sediments during diagenesis, in low- to granulite-grade metamorphic rocks, in migmatites, and is common in peraluminous igneous rocks. Xenotime can be a complement, or indeed an alternative, to monazite and/or zircon in geochemical and geochronological studies. To maximise the petrographic potential of xenotime, a complete understanding of its composition and relationship to rock-forming assemblages is essential. Electron beam techniques provide micron-scale resolution of compositional and textural variation and yield precise dates for individual micro-volumes in multi-domain grains. Methods for collecting trace element data by electron probe microanalysis differ from those routinely employed to collect major element concentrations. Careful characterisation of background curvature and background interferences around the Th, U and Pb peaks is required. To avoid large overlap correction for Y-Lγ2,3 on Pb-Mα, analysis of Pb is made on the Mβ-peak. A broad array of geochemical and geochronological applications can take advantage of the links between xenotime composition and texture and the evolution of silicate-mineral assemblages in a diversity of environments. One example of metasomatised xenotime from a pegmatite in SW Norway demonstrates a practical application to dating geologic processes, as well as the potential limitations that arise in compositionally heterogeneous xenotime.
AB - Xenotime (YPO4) is iso-structural with zircon-group minerals and lies at one end of a compositional solid-solution with monazite. As with monazite and zircon, naturally occurring xenotime may accommodate significant concentrations of rare earth elements, as well as Th and U, making it an important repository for these valuable geochemical marker elements and a potential geochronometer. Xenotime grows in sediments during diagenesis, in low- to granulite-grade metamorphic rocks, in migmatites, and is common in peraluminous igneous rocks. Xenotime can be a complement, or indeed an alternative, to monazite and/or zircon in geochemical and geochronological studies. To maximise the petrographic potential of xenotime, a complete understanding of its composition and relationship to rock-forming assemblages is essential. Electron beam techniques provide micron-scale resolution of compositional and textural variation and yield precise dates for individual micro-volumes in multi-domain grains. Methods for collecting trace element data by electron probe microanalysis differ from those routinely employed to collect major element concentrations. Careful characterisation of background curvature and background interferences around the Th, U and Pb peaks is required. To avoid large overlap correction for Y-Lγ2,3 on Pb-Mα, analysis of Pb is made on the Mβ-peak. A broad array of geochemical and geochronological applications can take advantage of the links between xenotime composition and texture and the evolution of silicate-mineral assemblages in a diversity of environments. One example of metasomatised xenotime from a pegmatite in SW Norway demonstrates a practical application to dating geologic processes, as well as the potential limitations that arise in compositionally heterogeneous xenotime.
KW - Electron microprobe
KW - Total Th-U-Pb dating
KW - Trace element analysis
KW - Xenotime
UR - http://www.scopus.com/inward/record.url?scp=49349093440&partnerID=8YFLogxK
U2 - 10.1016/j.chemgeo.2008.05.020
DO - 10.1016/j.chemgeo.2008.05.020
M3 - Article
AN - SCOPUS:49349093440
SN - 0009-2541
VL - 254
SP - 133
EP - 147
JO - Chemical Geology
JF - Chemical Geology
IS - 3-4
ER -