Titlebook: Integration of Earth Science Research on the Turkish and Greek 1999 Earthquakes; Naci Görür (President of Marmara Research Centre), Book 2

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Integration of Earth Science Research on the Turkish and Greek 1999 Earthquakes978-94-010-0383-4Series ISSN 1568-1238

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https://doi.org/10.1007/978-94-010-0383-4earthquake; fault; fault zone; geodesy; seismic; seismology; tectonics; tsunami

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Methods for Imaging Earthquake Deformation Using Satellite Data and Digital Elevation Models, (slip direction, amount) can be extracted. Remote sensing can also provide conclusive evidence towards identifying the surface expression of seismogenic structures during events between 5.5 and 6 M.. Data spatial resolution and sun angle are the dominant factors that influence mapping quality.

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Book 2002vents caused great concern among the earth science community. This book presents and discusses the latest results from studies of the Izmit-Düzce and Athens earthquakes and assesses the data that are available and relevant to the geology, seismology, tectonics, geodesy and other fields related to ea

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The Athens Earthquake September 7, 1999 Neotectonic Regime and Geodynamic Phenomena,ral morphotectonic structure of Attica and on data concerning the geological — alpine and post-alpine — formations and structure. It is shown that the regional stress field has to be more complicated than a pure extensional regime, so that the geometry and kinematics of the area are interpreted sufficiently.

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Earthquake Triggering in Greece and the Case of the 7 September 1999 Athens Earthquake,was found that the microseismicity of the Athens increased drastically immediately after the Izmit shock culminating with the main shock. It is suggested that ordinary (or triggering) earthquakes trigger distant microseismicity and this triggers secondary (or triggered) earthquake.