Geophysical and petrological modelling of the structure and composition of the crust and upper mantle in complex geodynamic settings: the Tyrrhenian Sea and …

GF Panza, A Peccerillo, A Aoudia, B Farina - Earth-Science Reviews, 2007 - Elsevier
Information on the physical and chemical properties of the lithosphere–asthenosphere
system (LAS) can be obtained by geophysical investigation and by studies of petrology …

Relative sea level changes and regional tectonic evolution of seven coastal areas in NW Greece since the mid-Holocene

A Vött - Quaternary Science Reviews, 2007 - Elsevier
This study presents relative sea level (RSL) curves for seven coastal areas in Akarnania and
the northwestern Peloponnese (NW Greece) since the mid-Holocene. RSL fluctuations are …

Seismic versus aseismic deformation in Iran inferred from earthquakes and geodetic data

F Masson, J Chéry, D Hatzfeld… - Geophysical Journal …, 2005 - academic.oup.com
A combined analysis of the geodetic strain-rate field and the strain-rate field deduced from
the seismicity allows us to define the style of deformation and to distinguish seismic from …

Crustal motion and deformation in Greece from a decade of GPS measurements, 1993–2003

C Hollenstein, MD Müller, A Geiger, HG Kahle - Tectonophysics, 2008 - Elsevier
The Hellenic plate boundary region, located in the collision zone between the
Nubian/Arabian and Eurasian lithospheric plates, is one of the seismo-tectonically most …

The Cephalonia transform fault and its extension to western Lefkada Island (Greece)

E Louvari, AA Kiratzi, BC Papazachos - Tectonophysics, 1999 - Elsevier
The central area of the Ionian Islands is dominated by the existence of a major tectonic
structure called the Cephalonia Transform Fault (CTF). Its main part (Cephalonia segment) …

Focal mechanisms of shallow earthquakes in the Aegean Sea and the surrounding lands determined by waveform modelling: a new database

A Kiratzi, E Louvari - Journal of Geodynamics, 2003 - Elsevier
Source parameters for 40 earthquakes with epicentres in the Aegean Sea and the
surrounding lands have been determined using P and SH body waveform inversion of …

GPS and geologic estimates of the tectonic activity in the Marmara Sea region, NW Anatolia

C Straub, HG Kahle, C Schindler - Journal of Geophysical …, 1997 - Wiley Online Library
A dense network of 52 Global Positioning System (GPS) sites is used to determine the
velocity field and strain rate pattern at the western end of the North Anatolian Fault Zone …

[HTML][HTML] The strain rate field in the eastern Mediterranean region, estimated by repeated GPS measurements

HG Kahle, C Straub, R Reilinger, S McClusky, R King… - Tectonophysics, 1998 - Elsevier
We use the combined GPS velocity field of the eastern Mediterranean for the period 1988 to
1996 to determine crustal deformation strain rates in a region comprising the Hellenic arc …

[PDF][PDF] Fault plane solutions in the Aegean Sea and the surrounding area and their tectonic implication

EK Louvari - Boll. Geof. teor. appl, 1998 - academia.edu
Fault plane solutions for 127 earthquakes, of magnitude M 2 55 and shallow focal depth (h-
60 km), which occurred in the Aegean Sea and surrounding area (34 N-43 N, 18 E-30" E) …

The Greek Database of Seismogenic Sources (GreDaSS): state-of-the-art for northern Greece

R Caputo, A Chatzipetros, S Pavlides… - Annals of …, 2012 - annalsofgeophysics.eu
Abstract The Greek Database of Seismogenic Sources (GreDaSS) is a repository of
geological, tectonic and active-fault data for the Greek territory and its surroundings. In this …