[HQR04-P05] Dating of hydrothermal silicified sediments by thermoluminescence
キーワード：熱ルミネッセンス年代測定、石英、熱水性珪化堆積物
The ages of hydrothermal activities are key issues in estimating the geothermal processes under the sea floor especially such as ore formation. Silicified sediments, widely distributed in hydrothermal fields of the sea floor, are potentially subject of trapped-charge dating, and their ages will contribute to the issues. Coarse and fine quartz grains were identified in the hydrothermal silicified sediments under a polarizing microscope. We tried thermoluminescence (TL) dating for each grain extracted from hydrothermal silicified sediments in the Okinawa Trough. We first checked the characteristics of silicified sedimentary quartz, such as TL peaks, wavelengths, and the dose response. The distribution of the radioactive elements was obtained by using imaging plates. As results of TL dating, coarse grains were found to be older than fine grains. Tentatively it is interpreted that coarse grains originated in volcaniclastic sediments have incompletely reset by hydrothermal activity, whereas fine grains precipitated from hydrothermal solutions, indicating the ages of the hydrothermal activities.