Dose Determination of Fluvial Sediments in Manisa

Müjde DURUKAN GÜLTEPE, Arzu Ege
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Abstract

Quartz, which is one of the most abundant minerals in nature, can be found in magmatic and metamorphic forms, as well as the usual components of granite and sedimentary formations. Quartz minerals, which are also known as the main component of quartzites, are also known as gangue minerals in many mineralizations. Quartz samples from two different sampling levels, namely the Kaletepe lower and the Kaletepe upper region, used in the study were prepared. Thermoluminescence (TL) glow curves of the samples exposed to radiation with a 90Sr/90Y β source were recorded with a TLD reader. While peaks were obtained at approximately 270 °C from the glow curves of the Kaletepe lower samples irradiated with β source, peaks were obtained at approximately 270 °C and 350 °C from the Kaletepe upper samples. When the annual average dose and age values of the lower and upper Kaletepe samples are examined, it can be said that it was formed in a time period of ~8000 years between two areas with a height difference of 130m.
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马尼萨冲积沉积物的剂量测定
石英是自然界中最丰富的矿物之一,可以在岩浆岩和变质岩中找到,也是花岗岩和沉积岩的常见成分。石英矿物也被称为石英岩的主要成分,在许多矿化过程中也被称为煤矸石矿物。研究中使用的石英样品来自两个不同的采样层,即卡莱特佩下层和卡莱特佩上层地区。用 TLD 阅读器记录了样品在 90Sr/90Y β 源辐射下的热释光(TL)辉光曲线。用 β 源辐照的 Kaletepe 下部样品的辉光曲线在大约 270 ℃ 出现峰值,而 Kaletepe 上部样品的辉光曲线在大约 270 ℃ 和 350 ℃ 出现峰值。如果对卡莱特佩下层和上层样品的年平均剂量和年龄值进行研究,可以说它是在高度相差 130 米的两个地区之间约 8000 年的时间内形成的。
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