The nucleation and rupture process of the 1981 Gulf of Corinth earthquakes from deconvolved broad‐band data

Geophysical Journal International

Volumn 120, Issue 2, 1995, Pages 393-405

  Abercrombie, R E ^a   Main, I G ^b   Douglas, A ^c   Burton, P W ^d  

^a UNIVERSITY OF READING   (United Kingdom)

^b UNIVERSITY OF EDINBURGH   (United Kingdom)

^c MINISTRY OF DEFENCE   (United Kingdom)

^d UNIVERSITY OF EAST ANGLIA   (United Kingdom)

Author keywords

Key words: Aegean, body waves, 2 D model, earthquake, rupture and nucleation.

Indexed keywords

GULF OF CORINTH EARTHQUAKES 1981; NORMAL FAULTING; NUCLEATION; RUPTURE PROCESS; SOURCE COMPLEXITY;

GREECE, GULF OF CORINTH;

EID: 0028812901     PISSN: 0956540X     EISSN: 1365246X     Source Type: Journal    
DOI: 10.1111/j.1365-246X.1995.tb01827.x     Document Type: Article

References (59)

1. S due to surface wave path effects
2. Local observations of a large earthquake: 28 June 1992 Landers, California
3. Surface strong motion associated with a stick‐slip event in a foam rubber model of earthquakes
4. Broadband modelling of the Corinth earthquakes of February and March 1981
5. Geodetic determination of tectonic deformation in central Greece from 1900 to 1988
6. Absorption of elastic waves—an operator for a constant Q mechanism
7. A quantitative evaluation of teleseismic explosion records
8. The rupture characteristics of two deep earthquakes inferred from broadband GDSN data
9. Broadband analysis of the extended foreshock sequence of the Miyagi‐Oki earthquake June 12, 1978
10. Direct measurement of the mantle attenuation operator from broadband P and S waveforms
11. b 6.0) earthquake: broadband body‐wave analysis of the north Yemen earthquake of 13 December 1982
12. Rupture process of an extended earthquake sequence: teleseismic analysis of the Chilean earthquake of March 3, 1985
13. Evidence for the variation of stress drop between normal and thrusting earthquakes in Italy
14. The effect of attenuation on seismic body waves
15. Why large earthquakes do not nucleate at shallow depths
16. Frequency dependence of Q in the mantle underlying the shield areas of Eurasia, Part III: the Q model
17. Time domain waveform inversion: a frequency domain view. How well do we need to match waveforms?
18. Q for short‐period P‐waves: is it frequency dependent?
19. A quantitative analysis of seismic signals at teleseismic distances—III. Computed P and Raleigh wave seismograms
20. Comments on ‘Analysis of broadband seismograms from the Chile‐Peru area, by R. Kind and D. Seidl’
21. Surface reflections and S‐to‐P conversions on P seismograms
22. Northern Chile earthquakes of 1980 May 26: evidence of unilateral fracture
23. L= 5.2)
24. An experiment in systematic study of global seismicity: centroid‐moment tensor solutions for 201 moderate and large earthquakes of 1981
25. Evidence of bias in estimations of earthquake size
26. The determination of the elastic field of an ellipsoidal inclusion and related problems
27. Dispersive body waves
28. Magnitude and energy of earthquakes
29. The rupture process of the Armenian earthquake from broad‐band teleseismic body wave records
30. A quantitative evaluation of seismic signals at teleseismic distances—I. Radiation from point sources
31. A quantitative evaluation of seismic signals at teleseismic distances—II. Body waves and surface waves from an extended source
32. The geometrical evolution of normal fault systems
33. The relationship between plate motions and seismic moment tensors, and the rates of active deformation in the Mediterranean and Middle East
34. Seismicity, normal faulting and the geomorphical development of the Gulf of Corinth: the Corinth earthquakes of February and March 1981
35. The energy release in great earthquakes
36. Source parameters of the 1981 Gulf of Corinth earthquake sequence from body‐wave analysis
37. The evolution of the Gulf of Corinth (Greece): an aftershock study of the 1981 earthquakes
38. Rupture characteristics of the 1982 Tonga and 1986 Kermadec earthquakes
39. The 1986 Kalamata (south Peleponnesus) earthquake: detailed study of a normal fault, evidence for east‐west extension in the Hellenic Arc
40. Active tectonics of the Alpine‐Himalayan, belt: the Aegean Sea and surrounding regions
41. Seismotectonics and the earthquake frequency—magnitude distribution in the Aegean area
42. Moment‐magnitude scaling in the Aegean area
43. Crustal structure of the central Aegean Sea, and the islands of Evia and Crete, Greece, obtained from refractional seismic experiments
44. The earthquake of April 10, 1954, in Sophades (Central Greece)
45. Properties of the February‐March 1981 seismic sequence in the Alkyonides gulf of central Greece
46. Radiation from a realistic model of faulting
47. Frictional constraints on thrust, wrench and normal faults
48. A source study of the Thessaloniki (northern Greece) 1978 earthquake sequence
49. Q and the rise and fall of a seismic pulse
50. Seismograms from phaseless seismographs
51. Active tectonics of the north and central Aegean Sea
52. The seismicity, geomorphology and structural evolution of the Corinth area of Greece
53. Rupture process of the Superstition Hills earthquake from the inversion of strong motion data
54. Rupture model of the 1989 Loma Prieta eqrthquake from the inversion of strong motion and broadband teleseismic data
55. Distributions of cumulative displacement and seismic slip on a single normal fault surface
56. Bathymetric effects on body waveforms from shallow subduction zone earthquakes and application to seismic processes in the Kurile trench