TY - JOUR
T1 - The strain field in northwestern Greece and the Ionian Islands
T2 - results inferred from GPS measurements
AU - Kahle, Hans Gert
AU - Müller, Max V.
AU - Geiger, Alain
AU - Danuser, Gaudenz
AU - Mueller, Stephan
AU - Veis, George
AU - Billiris, Harris
AU - Paradissis, Demitris
N1 - Funding Information:
In the 1989 campaign fourteen dual-frequency receiverso f the Wild-Magnavox1 02 type and in the 1993 campaign 14 Leica System 200 receiversw ere used. Apart from those of the ETH Ztirich, instruments were providedb y the National TechnicalU ni-versity of Athens, the Universitieso f Berlin, Karl-sruhe, Stuttgartt,h e Universityo f the Federal Armed Forces (FAF), Munich (Germany), the Technical University of Vienna (Austria), the Fachhochschule Stuttgart, the EPF Lausanne, Fa. Gester, Geneva (Switzerland),t he Agenzia Spaziale Italiana (ASI) and the Istituto Geografico Militare (IGMI). The valuable assistanceo f all these institutionsis gratefully acknowledgedW. e acknowledgew ith gratitude the support of the Hellenic Navy and the Hellenic Coast Guard for providing transportatiotno the island of Strofades.T he main funding agency of the research activities in western Greece is the Swiss Federal Institute of Technology (ETH ZUrich). We are very thankful for this support. In particularw e are indebtedt o Prof. R. Hiitter, Vice-Presidenotf the ETH ZiJrich, for his continuing help and advice. Additional financial support was provided by the NTU Athens.
PY - 1995/9/15
Y1 - 1995/9/15
N2 - Recent crustal movements detected by the analysis of repeated satellite geodetic measurements reflect the ongoing geodynamic processes in the Alpine-Mediterranean area. Superimposed on the large-scale counterclockwise rotation of the African plate, complex dynamic processes are affecting the lithospheric fragments between the African and Eurasian plates. Key features to better understand the driving forces and associated seismic activity in the Africa/Eurasia collision zone are the Calabrian and Hellenic arcs. In this paper geodynamic investigations along the West Hellenic arc are discussed. They are based on two epochs (1989 and 1993) of satellite geodetic measurements carried out using the US Global Positioning System (GPS). The results are presented in terms of relative displacements and strain rates. Within the time span of 4 years southwestern Greece has moved to the southwest relative to southeastern Italy by an average of 120 mm, increasing from 80 mm at Lefkada, in the center of the Ionian Islands, to 160 mm at the Peloponnesus. The maximum strain rate is 0.18 μstrain/a located in the vicinity of Lefkada, where anomalously high earthquake activity is observed. The data provide strong evidence for dextral strike-slip motion on the order of 25 mm/a along the Kephalonia Fault Zone (KFZ). The deformation field of the KFZ is interpreted as a transition zone between the kinematics of the Apulian platform and the West Hellenic fold and thrust belts.
AB - Recent crustal movements detected by the analysis of repeated satellite geodetic measurements reflect the ongoing geodynamic processes in the Alpine-Mediterranean area. Superimposed on the large-scale counterclockwise rotation of the African plate, complex dynamic processes are affecting the lithospheric fragments between the African and Eurasian plates. Key features to better understand the driving forces and associated seismic activity in the Africa/Eurasia collision zone are the Calabrian and Hellenic arcs. In this paper geodynamic investigations along the West Hellenic arc are discussed. They are based on two epochs (1989 and 1993) of satellite geodetic measurements carried out using the US Global Positioning System (GPS). The results are presented in terms of relative displacements and strain rates. Within the time span of 4 years southwestern Greece has moved to the southwest relative to southeastern Italy by an average of 120 mm, increasing from 80 mm at Lefkada, in the center of the Ionian Islands, to 160 mm at the Peloponnesus. The maximum strain rate is 0.18 μstrain/a located in the vicinity of Lefkada, where anomalously high earthquake activity is observed. The data provide strong evidence for dextral strike-slip motion on the order of 25 mm/a along the Kephalonia Fault Zone (KFZ). The deformation field of the KFZ is interpreted as a transition zone between the kinematics of the Apulian platform and the West Hellenic fold and thrust belts.
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U2 - 10.1016/0040-1951(95)00042-L
DO - 10.1016/0040-1951(95)00042-L
M3 - Article
AN - SCOPUS:0029544023
SN - 0040-1951
VL - 249
SP - 41
EP - 52
JO - Tectonophysics
JF - Tectonophysics
IS - 1-2
ER -