A new calibrated strategy for the U-Th-Pb dating of bastnasite by xenotime
Bastnaesite is an important mineral geochronometer to record the REE mineralization time for REE deposits. As the only reliable primary standard for in situ U-Th-Pb dating, bastnaesite K-9 is inhomogeneous and nearly out of supply. The accurate in situ U-Th-Pb dating of bastnaesite and its wide appl...
Saved in:
Published in | Journal of analytical atomic spectrometry Vol. 37; no. 12; pp. 2599 - 2614 |
---|---|
Main Authors | , , , , , , , |
Format | Journal Article |
Published |
30.11.2022
|
Online Access | Get full text |
Cover
Loading…
Summary: | Bastnaesite is an important mineral geochronometer to record the REE mineralization time for REE deposits. As the only reliable primary standard for
in situ
U-Th-Pb dating, bastnaesite K-9 is inhomogeneous and nearly out of supply. The accurate
in situ
U-Th-Pb dating of bastnaesite and its wide application are still constrained by the lack of reliable reference materials. Therefore, a potential primary standard was proposed and assessed in thirty-one ablation settings in this paper. The normalized
206
Pb/
238
U and
208
Pb/
232
Th ratios (
i.e.
,
206
Pb/
238
U and
208
Pb/
232
Th fractionation) of xenotime XN01 are respectively similar or slightly different from those of bastnaesite K-9 in most ablation settings. The average value (
i.e.
, calibration factor) of
206
Pb/
238
U and
208
Pb/
232
Th ratios for XN01 is consistent with those for K-9 with the offsets of <2.4% in the same ablation setting when using the ratio-of-the-mean intensity method for data reduction. Thus, the most obtained ages of K-9 calibrated by XN01 are consistent with its reference age of 118 ± 1 Ma with the offsets of <2%. Moreover, four typical bastnasite samples were analyzed in three normal ablation settings. Their respective U-Pb and Th-Pb ages calibrated by XN01 were consistent with those by K-9 within uncertainty. Because of high Th contents (>4500 ppm) and Th/U ratios (>400), the Th-Pb ages of these young samples are acceptable and agree well with their respective published Th-Pb ages within uncertainty. Therefore, the matrix effect between xenotime XN01 and bastnaesite can be neglected normally. Xenotime XN01 is more uniform than K-9 and can serve as a primary reference material for the
in situ
U-Th-Pb dating of bastnaesite. Moreover, bastnaesite Zagi has a sufficient reservoir, uniform Th-Pb, corrected U-Pb ages, and can serve as a secondary reference material for quality control.
Xenotime XN01 can serve as the primary standard for the accurate in situ U-Th-Pb dating of bastnasite in normal ablation settings. |
---|---|
Bibliography: | https://doi.org/10.1039/d2ja00233g Electronic supplementary information (ESI) available. See DOI |
ISSN: | 0267-9477 1364-5544 |
DOI: | 10.1039/d2ja00233g |