Abstract
A confocal set-up for three-dimensional (3D) micro X-ray fluorescence (micro-XRF) was used at the mySpot beamline at BESSY II, which allows compositional depth profiling for various applications. We present results obtained with a confocal 3D micro-XRF set-up for chemical age dating using the U, Th and Pb concentrations of monazite within rock thin sections. The probing volume was determined to be approximately 21 × 21 × 24 µm3 for W-La using an excitation energy of 19 keV. The relative detection limits particularly for Pb are below 10 ppm (for counting times of 1000 s). Therefore, this 3D micro-XRF set-up is suitable for dating of minerals with low Pb concentrations as long as all Pb is radiogenic, allowing spatial resolution comparable to ion microprobe or laser ablation techniques.
The set-up was tested on monazites that are well characterized by isotopic techniques and have a wide range of ages, varying from 20 Ma to 1.82 Ga. Reference materials (GM3, F6, 3345) can be reproduced within error. The spread in the ages of all points determined by 3D micro-XRF is within 8 % of the isotopic reference value. The average 3D micro-XRF dates reproduce the reference ages with discrepancies between 10 and 13 Ma which translate to deviations of 1-4 %. Younger monazite samples from the European Alps (Baceno2, Bi9801) show slightly older 3D micro-XRF dates than those determined by isotopic techniques and table-top micro-XRF on whole grains. We interpret this to be related to age heterogeneities smaller than the spatial resolution and/or contributions by common Pb, which is a limitation for this technique. The method was then applied to monazites of unknown age from sapphirine-bearing granulites originating from the Gruf Complex (Alps, N-Italy). The 3D micro-XRF mean date was determined as 33 ± 4.4 Ma (2s) and was verified by ID-TIMS techniques. This age can be reliably interpreted as the age of the high-temperature (HT) event because the monazites are included in and intergrown with HT minerals (sapphirine, high-Al orthopyroxene)
The set-up was tested on monazites that are well characterized by isotopic techniques and have a wide range of ages, varying from 20 Ma to 1.82 Ga. Reference materials (GM3, F6, 3345) can be reproduced within error. The spread in the ages of all points determined by 3D micro-XRF is within 8 % of the isotopic reference value. The average 3D micro-XRF dates reproduce the reference ages with discrepancies between 10 and 13 Ma which translate to deviations of 1-4 %. Younger monazite samples from the European Alps (Baceno2, Bi9801) show slightly older 3D micro-XRF dates than those determined by isotopic techniques and table-top micro-XRF on whole grains. We interpret this to be related to age heterogeneities smaller than the spatial resolution and/or contributions by common Pb, which is a limitation for this technique. The method was then applied to monazites of unknown age from sapphirine-bearing granulites originating from the Gruf Complex (Alps, N-Italy). The 3D micro-XRF mean date was determined as 33 ± 4.4 Ma (2s) and was verified by ID-TIMS techniques. This age can be reliably interpreted as the age of the high-temperature (HT) event because the monazites are included in and intergrown with HT minerals (sapphirine, high-Al orthopyroxene)
| Originalsprog | Engelsk |
|---|---|
| Tidsskrift | European Journal of Mineralogy |
| Vol/bind | 21 |
| Udgave nummer | 5 |
| Sider (fra-til) | 927–945 |
| ISSN | 0935-1221 |
| DOI | |
| Status | Udgivet - 2009 |
Emneord
- Det Natur- og Biovidenskabelige Fakultet