The 1960 Chile earthquake - Inversion for slip distribution from surface deformation

Details The 1960 Chile earthquake - Inversion for slip distribution from surface deformation The 1960 Chile earthquake - Inversion for slip distribution from surface deformation

Dec 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990geoji.103..589b&link_type=abstract

Geophysical Journal International (ISSN 0955-419X), vol. 103, Dec. 1990, p. 589-598. Research supported by Fondo de Desarrollo C

Mathematics

Logic

62

Earthquake Damage, Geological Faults, Sea Level, Surface Waves, Chile, Crustal Fractures, Deformation, Lithosphere

Scientific paper

Details of the 1960 Chile faulting are investigated as revealed by surface movements. Classical uniform slip models of earthquake faults are employed as well as more recently developed models that allow spatial variability of slip. Important fractures of the oceanic lithosphere bound the 1960 rupture and are proposed as a potential source of fault segmentation within the Chilean subduction zone.

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