Japan Geoscience Union Meeting 2015

Presentation information


Symbol M (Multidisciplinary and Interdisciplinary) » M-TT Technology & Techniques

[M-TT44] Frontiers in Geochemistry: Prospect for geochemistry in 30 years

Tue. May 26, 2015 6:15 PM - 7:30 PM Convention Hall (2F)

Convener:*Takafumi Hirata(Graduate School of Science, Kyoto University), Yoshio Takahashi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Urumu Tsunogai(Graduate School of Environmental Studies, Nagoya University), Hajime Obata(Marine inorganic chemistry division, Atmosphere and Ocean Research Institute, University of Tokyo), Shogo Tachibana(Department of Natural History Scieces, Hokkaido University), Katsuhiko Suzuki(Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology), Gen Shimoda(Geological Survey of Japan, AIST), Hiroyuki Kagi(Geochemical Laboratory, Graduate School of Science, University of Tokyo), Yusuke Yokoyama(Atmosphere and Ocean Research Institute, University of Tokyo), Tetsuya Yokoyama(Department of Earth and Planetary Sciences, Graduate School of Science and Engineering, Tokyo Institute of Technology)

6:15 PM - 7:30 PM

[MTT44-P03] Development of new ion collector for U-Pb Age cytometry

*Takafumi HIRATA1, Kentaro HATTORI1, Shuhei SAKATA1, Yuji ORIHASHI2 (1.Kyoto University, 2.Earth Research Institute, The University of Tokyo)

Age distribution (age cytometry) is one of the most principal and versatile information to decode the geological events underlying the Earth evolution. To take full advantage of the age cytometry, both the high analytical throughput and the better precision in the age determination is severely desired. Combination of laser ablation sampling technique and the high-sensitivity ICP-mass spectrometer (LA-ICPMS) enables us to measure precise U-Pb ages directly from the small area in the solid samples. Recently, both the precision and reliability of the U-Pb age data was dramatically improved by both the newly developed ion counting technique using the attenuator device and the correction technique for the initial disequilibrium for the U-Th-Pb decay series (Sakata et al., 2014). Moreover, magnetic sector-based mass spectrometry equipped with the multiple-ion counting system results in much higher analytical precision in the Pb/U and Pb/Th isotope ratio measurements. With the multiple-ion counting system, the analysis time for the U-Pb age determination could be dramatically shortened down to 1 - 5 sec, which was almost 1/4 - 1/10 levels over the conventional U-Pb age determinations using the single collector ICPMS instruments. This suggests that both the higher analytical throughput and the better precision in the Pb/U ratio measurements could be achieved. The problem associated with the multi-ion counting technique would be a time-dependent changes in the gain and the background (dark noise) of the multipliers. This is one of the large sources of analytical error in the U-Th-Pb age determinations. To overcome this, multiple-ion counting system using Daly ion collectors was employed in our MC-ICPMS system.

Several unique features could be achieved by the Daly ion counter, such as (a) wider dynamic range of the ion counting up to <10 Mcps, (b) smaller time-changes in gain and background level of the collector, and (c) better peak parallelism (peak flatness) over the conventional multipliers. Only the problem associated with the Daly counter is that the width of the Daly collector would be significantly larger than the mass dispersion for the heavier elements. In this study, two pairs of ion deflectors were used to obtain wider mass dispersion for the ion beams. With the multiple ion counting using the Daly ion counters, better precision and smaller contribution of the time-dependent changes in the gain and background counts could be achieved.

In this presentation, new ion collector system was applied to the MC-ICPMS system, and the preliminary results on the Pb/U and Pb/Th isotope ratio measurements and age determinations on zircon samples will be described.