THE FIRST RESULTS OF PALEOSEISMOLOGICAL RESEARCH ON THE ÇENDİK-YASSIGÜME SEGMENT OF BURDUR FAULT
Öz
Burdur-Fethiye Fault zone is an active zone and composed of different segments NE-SW directed. NE-SW directed system is 300 km in length and usually consist of the normal faults which have left oblique component. NE-SW directed Burdur graben has consist mainly Plio-Quaternary aged alluvium and lacustrinal sediment. In this region destructive earthquakes were occured in historical and instrumental periods. Especially earthquakes occuring in the years 1914 and 1971 are located on the Yassıgüme-Çendik segments of Burdur fault in SW. A trench is opened on the Burkent region between NE of Çendik and SW of Burdur and analyzed radiocarbon age. According to result of analysis surface rupture of earthquake in 1914 is observed. In this trench it is interpreted of detected another fault may be belong to earthquake in the year B.C. 53. In addition to, a tectonical event which occured surface rupture around of the years B.C. 2250 is detected in this trench.
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Kaynakça
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