Optically stimulated luminescence dating of Holocene alluvial fans, East Anatolian Fault System, Turkey

被引:3
|
作者
Dogan, Tamer [1 ]
Cetin, Hasan [2 ]
Yegingil, Zehra [3 ]
Topaksu, Mustafa [3 ]
Yuksel, Mehmet [3 ]
Duygun, Firat [4 ]
Nur, Necmettin [5 ]
Yegingil, Ilhami [6 ]
机构
[1] Cukurova Univ, Vocat Sch Imamoglu, Dept Comp Technol, TR-01700 Adana, Turkey
[2] Cukurova Univ, Dept Geol Engn, Fac Engn & Architecture, TR-01330 Adana, Turkey
[3] Cukurova Univ, Arts Sci Fac, Dept Phys, TR-01330 Adana, Turkey
[4] TUBITAK Marmara Res Ctr, Earth & Marine Sci Inst, TR-41400 Kocaeli, Turkey
[5] Adiyaman Univ, Dept Electir Elect Engn, Fac Engn, TR-02040 Adiyaman, Turkey
[6] Hasan Kalyoncu Univ, Fac Engn, TR-27000 Gaziantep, Turkey
来源
RADIATION EFFECTS AND DEFECTS IN SOLIDS | 2015年 / 170卷 / 7-8期
关键词
East Anatolian Fault System; D-SAR; OSL dating; equivalent dose; annual dose rate; POLYMINERAL FINE GRAINS; DOSE DISTRIBUTION ANALYSIS; SINGLE-ALIQUOT; FLUVIAL QUARTZ; GREEN LIGHT; SLIP-RATE; OSL; SEDIMENTS; TECTONICS; PLATE;
D O I
10.1080/10420150.2015.1077333
中图分类号
TL [原子能技术]; O571 [原子核物理学];
学科分类号
0827 ; 082701 ;
摘要
In this study, the optically stimulated luminescence dating technique was used to determine the time of deposition of alluvial sediment samples from the Turkoglu-Antakya segment of the East Anatolian Fault System (EAFS) in Turkey. The double-single aliquot regenerative dose protocol on fine grain samples was used to estimate equivalent doses ( De). Annual dose rate was computed using elemental concentration of uranium ( U) and thorium ( Th) determined by using thick-source alpha counting and potassium (K) concentrations using X-ray fluorescence and/or atomic absorption spectroscopy. The environmental dose was measured in situ using alpha- Al(2)O3: C chips inside plastic tubes for a year. The two different bulk sediment samples collected from the Islahiye trench yielded ages of 4.54 +/- 0.28 and 2.91 +/- 0.23 ka. We also obtained a 2.60 +/- 0.18 ka age for the alluvial deposit in the Kiranyurdu trench and 2.31 +/- 0.14 ka age for an excavation area called Malzeme Ocagi. These ages were consistent with the corresponding calibrated Carbon- 14 ( 14C) ages of the region. The differences between the determined ages were insufficient to clearly distinguish the disturbance event from the effects of bioturbation, biological mixing, or other sources of De variation in the region. They provide a record of alluvial aggradation in the region and may determine undocumented historical earthquake events.
引用
收藏
页码:630 / 644
页数:15
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