用光激发发光法测定沉积物样品的年龄

I. Sandeva
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引用次数: 0

摘要

发光测年是一种重要的年龄测定方法,它是基于对沉积物和人工制品中最常见的矿物石英和长石的发光特性的研究。这种测年方法的最大优点是它的动态范围很广,从10年到50万年不等,而且它能够应用于许多不同的材料和各种粒度,从细缝到中砂。本文采用光激发发光技术对沉积物样品进行了测量,包括样品制备和结果分析
本文章由计算机程序翻译,如有差异,请以英文原文为准。
AGE DETERMINATION OF A SEDIMENT SAMPLE BY OPTICALLY STIMULATED LUMINESCENCE
A b s t r a c t: Luminescence dating is an important method for age determination that is based on studying the luminescence characteristics of quartz and feldspar as the most common minerals in sediments and artifacts. The greatest advantage of this dating method is its wide dynamic range, starting from 10 years to 500000 years and its ability to be applied on many different materials and to a range of grain sizes, from fine slit to medium sand. Measurements in this paper are done on sediment samples by optically stimulated luminescence technique, including sample preparation and analysis of results
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