کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
1040180 1484097 2016 12 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Beachrock formation on the coast of Gökçeada Island and its relation to the active tectonics of the region, northern Aegean Sea, Turkey
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات زمین شناسی
پیش نمایش صفحه اول مقاله
Beachrock formation on the coast of Gökçeada Island and its relation to the active tectonics of the region, northern Aegean Sea, Turkey
چکیده انگلیسی

There are beachrock formations in 5 different sections of the south coast of Gökçeada, Turkey's largest Aegean island. These beachrocks form two different groups in terms of layering characteristics, δ18O and δ13C stable isotope compositions, consecutive cementation structures, and 14C dating. The West Group beachrocks, to the west, were dated to 4010–5830 BP, while the East Group beachrocks were dated to 620–2390 BP. The beachrock formations in both groups are separated by the NE–SW-trending Uğurlu Fault. The Uğurlu Fault is a right lateral, strike slip with reverse component oblique fault, and is an active fault within the North Anatolian Fault Zone. In the period between the formation of the two beachrock groups (2390–4010 BP), an earthquake was responsible for the destruction of Gökçeada Yenibademli mound and the development of two generations of beachrock.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Quaternary International - Volume 401, 16 May 2016, Pages 141–152
نویسندگان
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