Japan Geoscience Union Meeting 2014

Presentation information

Oral

Symbol S (Solid Earth Sciences) » S-GL Geology

[S-GL42_29AM2] Geochronology and Isotope Geology

Tue. Apr 29, 2014 11:00 AM - 12:45 PM 419 (4F)

Convener:*Takahiro Tagami(Graduate School of Science, Kyoto University), Yuji Sano(Division of Ocean and Earth Systems, Atmosphere and Ocean Research Institute, University of Tokyo), Chair:Yuji Sano(Division of Ocean and Earth Systems, Atmosphere and Ocean Research Institute, University of Tokyo), Takahiro Tagami(Graduate School of Science, Kyoto University)

11:55 AM - 12:10 PM

[SGL42-10] LA-ICP-MS U-Pb dating of Oki Dozen volcano using non-polished zircons

*Hisatoshi ITO1, Marco BRENNA2, Daisuke MIURA1, Kiyoshi TOSHIDA1, Setsuya NAKADA2 (1.CRIEPI, 2.Univ. of Tokyo)

Keywords:U-Pb dating, zircon, LA-ICP-MS, Oki Dozen volcano

LA-ICP-MS U-Pb dating using zircon is now widely used with great success. The normal dating process includes polishing zircons. This process is good in terms of avoiding surface contamination of common Pb and/or Pb loss and is essential for SHRIMP, in which only small fraction (drilling depth of 1-2 μm) is used for dating. Compared to SHRIMP, LA-ICP-MS ablates a much larger volume (drilling depth of >10 μm) of zircon. This means that it is easy to date zircons from the surface to the inner core of the crystal and examine the existence of inherited cores and potentially investigate the timespan of crystallization. Here we dated non-polished zircons for some reference samples (Fish Canyon Tuff and OD-3) and samples from Oki Dozen volcano. Zircons were ablated for 30 seconds using 213 nm Nd-YAG laser with 10 Hz repetition rate and 4-5 J/cm2 energy density. Final drilling depth for 5 J/cm2 was 27 μm and the 206Pb/238U ratio from 9-18μm depth were used to determine ages. It was found that non-polished zircons yield reliable ages because of agreement with reference ages. The Oki Dozen samples yielded 6-7 Ma ages, in agreement with or slightly older than K-Ar ages of 5.4-7.4 Ma.