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Oral presentation

Potential of multiple mineral age standard; Preliminary study of the NST zircon from the Nisatai Formation in NE Japan

Nagata, Mitsuhiro; Fukuda, Shoma; Sueoka, Shigeru; Yokoyama, Tatsunori; Kagami, Saya; Niki, Sota*; Iwano, Hideki*; Danhara, Toru*; Ogita, Yasuhiro; Kajita, Yuya*; et al.

no journal, , 

no abstracts in English

Oral presentation

Development of zircon U-Th disequilibrium dating for determination of the eruption age of Zenikame-Menagawa tephra

Kagami, Saya; Yokoyama, Tatsunori; Niki, Sota*; Sakata, Shuhei*; Umeda, Koji*; Okada, Rina*; Kondo, Misaki*

no journal, , 

Tephras from submarine eruptions are easily affected by secondary deposition and alteration and the constraints on their geochronology may be difficult. In this study, we conducted zircon U-Th disequilibrium dating by LA-ICP-MS for Zenikame-Menagawa tephra (Z-M), which was erupted from Zenakame volcano on the seafloor of the Tsugaru Strait and is a valid age indicator for MIS3. The zircons in the Toya pumice were measured to evaluate the accuracy of the method and their isochron age of 128 ka was obtained. This result is consistent with the previous reported data by the same method used in this study. We measured the zircons from Z-M and found that many of the zircons did not record eruption ages, and that many grains had U-Th disequilibrium model ages of about 100 ka. In the future, we will attempt U-Th disequilibrium dating of each zircon along with understanding its characteristics (shape, chemical composition and so on).

Oral presentation

Electric quadrupole moment measurement using a new RF-application system

Nagae, Daisuke; Takemuara, Makoto*; Ueno, Hideki*; Kameda, Daisuke*; Asahi, Koichiro*; Yoshimi, Akihiro*; Sugimoto, Takashi*; Nagatomo, Takashi*; Kobayashi, Yoshio*; Uchida, Makoto*; et al.

no journal, , 

An electric quadrupole moment ($$Q$$ moment) is sensitive to collective aspects of nuclear structure. In the $$Q$$-moment measurement for unstable nuclei, we employ the $$beta$$-detected nuclear-quadrupole resonance method. In this method, we need to supply $$2I$$ resonance frequencies, where $$I$$ denotes the nuclear spin. We have developed a new RF-application system to induced all of the $$2I$$ transitions. The application of the $$2I$$ frequencies may be pursued in two different ways; the sequential RF pulse method and the mixed-wave RF pulse method. We confirmed the reversal of polarization for the both methods, from measurements of $$beta$$-ray asymmetry change for polarized $$^{12}$$B. Using this system, the $$Q$$ moments of $$^{31,32}$$Al have been measured to be $$|Q(^{31}{rm Al})| = 104(9)$$ $$e$$$$cdot$$mb and $$|Q(^{32}{rm Al})| = 24(2)$$ $$e$$$$cdot$$mb by the sequential RF pulse method.

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