参考剖面Yar Sredny(中部堪察加)“交叉层状砂质”地层的年龄根据泥炭的230 /238U和14C配对定年

F. Maksimov, Ф Е Максимов, M. Pevzner, М М Певзнер, A. Petrov, А.Ю. Петров, S. Levchenko, С Б Левченко, V. Grigoriev, Василий Александрович Григорьев, N. Baranova, Н. Г. Баранова, V. Kuznetsov, В. Ю. Кузнецов
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引用次数: 0

摘要

首次对堪察加中部松散沉积物中新更新世参考剖面中普遍存在的“交叉层状砂质”地层进行了数值放射性同位素测年。研究了两个泥炭层,它们被合并在亚尔沙河的“交叉层状砂质”地层中。2330 /238U和14C测年结果吻合较好。根据测年结果,确定了“交叉层状砂质”地层的沉积时间显然在5 -4万年前,即晚更新世(MIS-3),而不是之前认为的40 -30万年前的中更新世。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Age of the «cross-laminated sandy» stratum from the reference section Yar Sredny (Central Kamchatka) according to the paired 230Th /238U and 14C dating of peat
For the first time, numerical radioisotope age were obtained for the “cross-laminated sandy” stratum, which is widespread in Neopeopleistocene reference sections of loose sediments from Central Kamchatka. Two peat layers, incorporated in the “cross-laminated sandy” stratum of the Yar Sredny, were studied. The results of their paired 230Th/238U and 14C dating are in good agreement with each other. According to the dating results, it was determined that the “cross-laminated sandy” stratum was deposited, apparently, in the range of about 50-40 thousand years ago, i.e. in the Late Pleistocene (MIS-3), and not in the Middle Pleistocene, about 400-300 thousand years ago, as previously thought.
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