Historical evidence of faulting in Eastern Anatolia and Northern Syria
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Abstract
Historical data show that like the North Anatolian fault zone, which was delineated by a series of earthquakes during this century from east to west, so was the conjugate Eastern Anatolian fault zone delineated from the northeast to the southwest by a succession of large earthquakes in earlier times, with a major event at its junction with the Dead Sea fault system. This event was associated with surface faulting and occurred in a region seismically quiescent for nearly two centuries.
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Ambraseys NN, Melville CP. Historical evidence of faulting in Eastern Anatolia and Northern Syria. Ann. Geophys. [Internet]. 1995Nov.25 [cited 2022Jun.25];38(3-4). Available from: https://www.annalsofgeophysics.eu/index.php/annals/article/view/4110
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