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Source Characteristics of the January 8, 2013 (M w = 5.7) and May 24, 2014 (M w = 6.8) North Aegean Earthquakes Sequence

  • 2018
  • OriginalPaper
  • Chapter
Published in:
Authors
Doğan Kalafat
Kıvanç Kekovalı
Ali Pınar
Published in
Moment Tensor Solutions
Publisher
Springer International Publishing

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Abstract

The Aegean Sea, is one of the most seismically active areas of the Eastern Mediterranean region (Fig. 1). Generally, North Aegean Sea region has been tectonically developed after the collision of Arabian plate with the Eurasian in the Late Miocene time and the subsequent westward escape of the Anatolian Plate relative to the Eurasian Plate, during the Early Pliocene.

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previous chapter Intraplate Earthquakes in Europe—Source Parameters from Regional Moment Tensor Analysis
next chapter Investigating the Focal Mechanisms of the August 4th, 2003, 7.6, South Orkney Islands Earthquake and its Aftershocks Sequence
Title
Source Characteristics of the January 8, 2013 (M w = 5.7) and May 24, 2014 (M w = 6.8) North Aegean Earthquakes Sequence
Authors
Doğan Kalafat
Kıvanç Kekovalı
Ali Pınar
Copyright Year
2018
Book
Moment Tensor Solutions

Print ISBN: 978-3-319-77358-2

Electronic ISBN: 978-3-319-77359-9

Copyright Year: 2018

DOI
https://doi.org/10.1007/978-3-319-77359-9_16
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