Open AccessLocal and regional components of western Aegean deformation extracted from 100 years of geodetic displacement measurements
Author(s) -
Curtis Andrew,
England Philip,
Davies Robert
Publication year - 1997
Publication title -
geophysical journal international
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0956-540X
DOI - 10.1111/j.1365-246x.1997.tb01857.x
Subject(s) - geodetic datum , induced seismicity , geology , geodesy , deformation (meteorology) , seismology , displacement field , stress field , displacement (psychology) , geometry , mathematics , finite element method , psychology , oceanography , psychotherapist , physics , thermodynamics
SUMMARY Our objectives are as follows. First, we wish to develop a methodology to recover the long‐term component of deformation from any set of distributed, time‐averaged geodetic strain measurements that were subject to seismic disturbance, given a catalogue of local seismicity that occurred during the measurement period. Second, using seismic and geodetic data sets that span approximately 100 years, we apply this technique in the western Aegean to assess the role of local seismicity in regional deformation. The methodology is developed using a model for crustal deformation constructed from a long‐term, smooth regional strain field combined with instantaneous, local perturbations from upper‐crustal earthquakes approximated by static elastic dislocations. By inverting geodetic displacements for the smooth field while simultaneously floating influential but uncertain earthquake source parameters, an estimate of the regional component of deformation that is approximately independent of the seismicity can be made. In the western Aegean we find that the horizontal component of regional deformation can be described with minor inaccuracy by a quadratic relative displacement field. The principal horizontal extensional axes calculated from the regionally smooth displacement field agree in orientation with the T‐axes of earthquakes in the region. These observations indicate that the instantaneous elastic strain of the 10 km thick seismogenic layer is driven by a stress field that is smooth on the scale of the geodetic network as a whole, 200‐300 km.