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Bala (Ankara) Earthquakes: Implications for Shallow Crustal Deformation in Central Anatolian Section of the Anatolian Platelet (Turkey)
Bala (Ankara) Earthquakes Shallow Crustal Deformation Central Anatolian Section of the Anatolian Platelet
2010/10/14
Central Anatolia is quiet in terms of seismic activity, and rarely earthquakes up to magnitude 5.6 occur in the inner part of the Anatolian block or Anatolian platelet. Southeast of Ankara, the capita...
Distributed power-law seismicity changes and crustal deformation in the SW Hellenic ARC
power-law seismicity changes crustal deformation SW Hellenic ARC
2009/12/11
A region of definite accelerating seismic release rates has been identified at the SW Hellenic Arc and Trench system, of Peloponnesus, and to the south-west of the island of Kythera (Greece). The iden...
Investigation of long period crustal deformation on the inactive branch of the North Anatolian Fault Zone
long period crustal deformation inactive branch North Anatolian Fault Zone
2009/12/8
The western part of North Anatolian Fault (NAF) bifurcates around Mudurnu into two fault segments: northern and southern branch. The latter bifurcates again at west of Pamukova and creates middle stra...
Investigation of long period crustal deformation on the inactive branch of the North Anatolian Fault Zone
long period crustal deformation inactive branch North Anatolian Fault Zone
2009/12/16
The western part of North Anatolian Fault (NAF) bifurcates around Mudurnu into two fault segments: northern and southern branch. The latter bifurcates again at west of Pamukova and creates middle stra...
Crustal deformation and AE monitoring:annual variation and stress-soliton propagation
Crustal deformation AE monitoring annual variation stress-soliton propagation
2009/12/30
The stress propagation through the crust can be effectively monitored by means of acoustic mission (AE) techniques (ultrasounds). The \textit{AE} intensity is indicative of the amount of stress that a...