Absolute far-field displacements from the 28 June 1992 Landers earthquake sequence
Displacements observed for the Landers earthquake indicate that the depth of the bottom of the rupture is shallower towards the northern end. Displacements were dominantly symmetric and the rupture extended farther south on the Johnson Valley fault than has been mapped on the basis of surface ground...
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| Veröffentlicht in: | Nature (London) 1993-01, Vol.361 (6410), p.340-342 |
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| container_issue | 6410 |
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| container_title | Nature (London) |
| container_volume | 361 |
| creator | Blewitt, Geoffrey Heflin, Michael B. Hurst, Kenneth J. Jefferson, David C. Webb, Frank H. Zumberge, James F. |
| description | Displacements observed for the Landers earthquake indicate that the depth of the bottom of the rupture is shallower towards the northern end. Displacements were dominantly symmetric and the rupture extended farther south on the Johnson Valley fault than has been mapped on the basis of surface ground offsets. The combined geodetic moment for the Landers and Big Bear earthquakes agrees well with teleseismic estimates. |
| doi_str_mv | 10.1038/361340a0 |
| format | Article |
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| identifier | ISSN: 0028-0836 |
| ispartof | Nature (London), 1993-01, Vol.361 (6410), p.340-342 |
| issn | 0028-0836 1476-4687 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_25960272 |
| source | SpringerLink Journals; Nature; NASA Technical Reports Server |
| subjects | Earth sciences Earth, ocean, space Earthquakes Exact sciences and technology Geophysics Internal geophysics Plate tectonics Seismic activity Seismology Solid-earth geophysics, tectonophysics, gravimetry |
| title | Absolute far-field displacements from the 28 June 1992 Landers earthquake sequence |
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