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Revised ages of late Holocene tephras in Beppu Bay, central Kyushu, southwest Japan

机译:日本西南部九州中部别府湾晚全新世特非拉斯的年龄修订

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In this study, we revised eruptive ages, especially the Aso and Yufu volcanoes, central Kyushu, by analyzing a sediment core of southwestern Beppu Bay, southwest Japan, where undisturbed sediments are continuously deposited in a dysoxic basin. We identified two ash-fall layers in the sequence covering the last ca. 3000 years by using the refractive index of volcanic glasses and other parameters. These layers were likely correlated with N2 ash of the Aso volcano and Yufu-dake 1 ash (Yf1) of the Yufu volcano on the basis of the refractive indices of volcanic glasses, heavy mineral compositions, special distribution, and facies. According to high precision age models, the eruptive ages (68.2% probability range) of these tephras were 1470-1490 and 2010-2100 cal yr BP, respectively, and concordant with reported ages of previous research. These precise ages of tephras improve linking or dating in the various environments, and contribute to investigation of environmental changes or sedimentary process from source to sink. (C) 2017 Elsevier Ltd and INQUA. All rights reserved.
机译:在这项研究中,我们通过分析日本西南部别府湾西南部的沉积岩芯(其中未扰动的沉积物不断沉积在一个缺氧盆地中)来修订了九州中部的阿苏和由布火山的喷发年龄。我们在覆盖最后一个ca的序列中确定了两个降灰层。通过使用3000年火山玻璃的折射率等参数。根据火山玻璃的折射率,重矿物组成,特殊分布和相,这些层可能与阿苏火山的N2灰和由布火山的由布-达克1灰(Yf1)相关。根据高精度年龄模型,这些特弗拉斯的爆发年龄(68.2%概率范围)分别为BP年龄1470-1490和2010-2100 cal yr,与先前研究的报道年龄一致。这些精确的提弗拉斯年龄可以改善各种环境中的联系或年代,并有助于调查从源头到汇点的环境变化或沉积过程。 (C)2017爱思唯尔有限公司和INQUA。版权所有。

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