36Cl exposure ages of alluvial limestone boulders, near Yenice, Karabük, northern Turkey

An alluvial fan formed in the Filyos River Valley, resulting from landslide and fluvial activity in the Şimşir River. Debris flows were transported through Şeker Canyon and into the Filyos River Valley, creating an alluvial fan. The alluvial layers overly older fluvial fill terrace layers. Chemical preparations were performed at the İTÜ Kozmo-Lab in Istanbul, Turkey. The final AgCl targets were sent to the CNRS-ASTER, Aix en Provence, France for measurements using Accelerated Mass Spectrometry. Major and trace element concentrations of aliquots were measured at AcmeLabs, Canada.本数据集的研究对象为形成于菲利奥斯河（Filyos River）河谷的冲积扇（alluvial fan），其成因系希姆希尔河（Şimşir River）流域的滑坡与河流活动共同作用。碎屑流经由谢克尔峡谷（Şeker Canyon）搬运并汇入菲利奥斯河河谷，进而形成该冲积扇。冲积层覆于年代更古老的河流充填阶地地层之上。化学制备工作于土耳其伊斯坦布尔的伊斯坦布尔科技大学（İTÜ）科兹莫实验室（Kozmo-Lab）完成。最终的氯化银（AgCl）靶件被运送至法国普罗旺斯地区艾克斯的法国国家科学研究中心-阿斯特尔实验室（CNRS-ASTER），采用加速质谱法（Accelerated Mass Spectrometry）开展测试分析。等分试样的常量与微量元素浓度测定工作由加拿大AcmeLabs实验室完成。