The June 9 Bolivia and March 9 Fiji deep earthquakes of 1994: I. Source processes

Geophysical Research Letters

Volumn 22, Issue 16, 1995, Pages 2241-2244

  Lundgren, Paul ^a   Giardini, Domenico ^b  

^a CALIFORNIA INSTITUTE OF TECHNOLOGY   (United States)

^b ROMA TRE UNIVERSITY   (Italy)

Author keywords

[No Author keywords available]

Indexed keywords

BOLIVIAN EARTHQUAKE 1994; DEEP EARTHQUAKE; EARTHQUAKE SOURCE; FIJI EARTHQUAKE 1994;

EID: 0029527683     PISSN: 00948276     EISSN: 19448007     Source Type: Journal    
DOI: 10.1029/95GL02233     Document Type: Article

References (21)

1. Variation of seismic source parameters and stress drops within a descending slab and its implications in plate mechanics
2. On the limits of linear moment tensor inversion of surface wave spectra
3. Preliminary Reference Earth Model (PREM)
4. Teleseismic analysis of the great 1994 Bolivia earthquake, EOS
5. Source process of a large deep‐focus earthquake and its tectonic implications — the western Brazil earthquake of 1963
6. Source retrieval for mantle earthquakes by iterative deconvolution of long‐period P‐waves
7. Frequency distribution and quantification of deep earthquakes
8. Moment tensor inversion from MedNet data: (1) large worldwide earthquakes of 1990
9. The June 9 Bolivia and March 9 Fiji deep earthquakes of 1994: II. Geodynamic implications
10. Deep seismicity and modes of deformation in Tonga subduction zone
11. A new self‐organizing mechanism for deep‐focus earthquakes
12. Determination of the isotropic component of the 1994 Bolivia deep earthquake
13. Insignificant isotropic component in the moment tensor of deep earthquakes
14. Iterative deconvolution of complex body waves from great earthquakes — the Tokachi‐Oki earthquake of 1968
15. Inversion of complex body waves — III
16. The mechanism of the deep Bolivia earthquake of June 9, 1994
17. Mantle phase changes and deep‐earthquake faulting in subducting lithosphere
18. Seismicity, shear failure and modes of deformation in deep subduction zones
19. The rupture process and asperity distribution of three great earthquakes from long‐period diffracted P‐waves
20. A deep earthquake aftershock sequence and implications for the rupture mechanism of deep earthquakes