首页> 外文期刊>Journal of Coastal Research: An International Forum for the Littoral Sciences >Optical stimulated luminescence dating study of eolianite on the Island of Bozcaada, Turkey: Preliminary results
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Optical stimulated luminescence dating study of eolianite on the Island of Bozcaada, Turkey: Preliminary results

机译:土耳其博兹卡阿达岛上风云母的光学激发发光测年研究:初步结果

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摘要

In the present paper, eolianite exposed on the south coast of the semiarid island of Bozcaada, Turkey, was investigated on the basis of geomorphologic and petrographic data, and optically stimulated luminescence (OSL) dating results. The eolianite is lithic arenite in composition and contains abundant quartz, calcite, and various lithoclasts amalgamated with micritic calcite, sparitic calcite, and meniscus cements. Within the youngest layers standing at 12m above sea level, the rock contains rhizoliths with or without carbonaceous fills. The OSL ages obtained ranged between 24.21 ± 1.53ka and 16.18 ± 1.70ka, suggesting that eolianite constitutes an example of low stand deposits coinciding with oxygen isotope stage 2 (OIS-2).
机译:在本文中,根据地貌和岩石学数据,对暴露于土耳其博兹卡阿达半干旱岛南海岸的风成岩进行了研究,并得出了光激发发光(OSL)测年结果。钙长石是组成上的岩质陨石,含有大量的石英,方解石和各种由碎屑方解石,Sparitic方解石和弯液面水泥组成的碎石碎屑。在海拔12m的最年轻层中,岩石中含有带或不带碳质填充物的根茎。获得的OSL年龄介于24.21±1.53ka和16.18±1.70ka之间,这表明风云母构成了与氧同位素阶段2(OIS-2)相吻合的低层沉积物。

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