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Equivalent dose distribution analysis of Holocene eolian and fluvial quartz sands from Central Oklahoma

机译:俄克拉荷马州中全新世风成岩和河流石英砂的当量剂量分布分析

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摘要

Holocene quartz sands were collected from fluvial terrace deposits and eolian dune deposits adjacent to the North Canadian and Cimarron Rivers and their tributaries in Central Oklahoma. Single aliquot regenerative dose optically stimulated luminescence techniques were employed to generate equivalent dose (ED) distribution histograms for each sample. We hypothesize that the ED distributions are convolutions of the distribution arising from natural sedimentary processes, influenced primarily by the degree of solar resetting experienced by individual grains, and a distribution due to experimental error. An estimation of the experimental error distribution for each sample was made and this was then deconvolved from the experimentally measured ED distribution to reveal the 'sedimentary process' ED distribution. Objective methods for determining EDs, uncertainties, and confidence parameters from the deconvolved distributions are presented. (C) 2000 Elsevier Science Ltd. All rights reserved. [References: 10]
机译:全新世石英砂是从北加拿大河和Cimarron河及其在俄克拉荷马州中部的支流附近的河流阶地沉积物和风沙丘沉积物中收集的。采用单一等分试样的再生剂量光学激发发光技术为每个样品生成等效剂量(ED)分布直方图。我们假设ED分布是自然沉积过程产生的分布的卷积,主要受单个谷物经历的太阳复位程度以及实验误差引起的分布的影响。对每个样品的实验误差分布进行估算,然后将其与实验测量的ED分布进行反卷积,以揭示“沉积过程” ED分布。提出了从反卷积分布中确定ED,不确定性和置信度参数的客观方法。 (C)2000 Elsevier ScienceLtd。保留所有权利。 [参考:10]

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