Rupture zones and active crustal deformation in southern Thessalia, central Greece

B. C. Papazachos, P. M. Hatzidimitriou, G. F. Karakaisis, C. B. Papazachos, G. N. Tsokas

Research output: Contribution to journalArticlepeer-review

13 Scopus citations

Abstract

The southern Thessalia fracture belt has been selected as an area for pilot multinational studies on short term earthquake prediction. Thus, geophysical information has been used to accurately define the rupture zones of the three strongest earthquakes in this belt during the present century (1954 M = 7.0, 1957 M = 6.8, 1980 M = 6.5). Reliable fault plane solutions and seismic moment release rates have been used to show that the upper crust in this belt is seismically extending at a rate of 7 mm/yr in a N 6°W direction, and is vertically thinning at a rate of 3 mm/yr, which is in full agreement with normal faulting striking in a N 80°E direction. -from Authors

Original languageEnglish
Pages (from-to)363-374
Number of pages12
JournalBollettino di Geofisica Teorica ed Applicata
Volume35
Issue number139
StatePublished - 1993

ASJC Scopus subject areas

  • Oceanography
  • Geophysics

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