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Isotope fractionations and radiocarbon ages of beach rock samples collected from the Nansei Islands, southwest of Japan

机译:来自日本西南部的Nansei群岛收集的海滩岩石样品的同位素分级和辐射碳碳

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Four hundred and twelve beach rock samples were collected from 157 sites on 29 islands consisting of the Nansei Islands, in the southwestern part of Japan. They were radiocarbon dated and their isotope fractionations (δ~(13)C) were analyzed. The values of isotope fractionations of different materials making up the beach rocks ranged between +9.4 per thousand and —6.0 per thousand with an average of 1.99 per thousand. The isotope fractionations outside the range of 0 ± 2 per thousand suggest that these beach rocks were subjected to the influence of meteoric water when they cemented. Radiocarbon ages suggest that beach rocks in the Nansei Islands began to form about 6,900 yr BP and some of them are at present still under development at the islands.
机译:从29个岛屿的157个地点收集了四百和十二个海滩样本,该岛屿由日本西南部的Nansei岛组成。它们是radiocarbon的日期,分析它们的同位素分级(δ〜(13)c)。构成海滩岩石的不同材料的同位素分馏的值范围在+ 9.4‰之间,平均每千平方为1.99%。在0±2‰的范围之外的同位素分级表明,这些海滩岩石在粘接时受到易患的影响。 RadioCarbon Ages表明,NanSei岛上的海滩岩石开始形成约6,900亿亿桶,其中一些人目前仍在岛上开发。

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