control of seafloor roughness on earthquake rupture behavior: costa rica
DESCRIPTION
Control of Seafloor Roughness on Earthquake Rupture Behavior: Costa Rica. Susan Bilek University of Michigan. Detailed examination of Costa Rica subduction zone -- Large earthquake rupture and seismicity limits. Asperity Model for Large Earthquake Rupture. After Lay et al., 1982. - PowerPoint PPT PresentationTRANSCRIPT
Control of Seafloor Roughness on Earthquake Rupture Behavior:
Costa Rica
Susan Bilek
University of Michigan
Detailed examination of Costa Rica subduction zone
-- Large earthquake rupture and seismicity limits
Asperity Model for Large Earthquake Rupture
After Lay et al., 1982
CRSEIZE Experiment
PIs:
Schwartz (UCSC),
Protti (UNA-OVSICORI),
Dorman (USCD),
Dixon (Miami),
Lundgren (JPL)
Analysis of Large Earthquake Rupture - Aug 20, 1999 Mw 6.9 Underthrusting
Earthquake
• One of the largest earthquakes in this segment of margin
• Occurred shortly before temporary network deployment -- opportunity for
recording aftershocks
• Occurred in region of disrupted subducted crust (Quepos Plateau)
Surface Wave AnalysisAug 20, 1999 Mw 6.9
Earthquake
RSTF durations, azimuths related to true duration, rupture direction
Search over all azimuths, find most linear fit between duration & directivity parameter best rupture azimuth
Empirical Green’s function deconvolution method using surface waves -- remove path and instrument effects, leave information about source
P wave inversion results - 1999 Osa Earthquake
Rupture Process of 1999 Mw 6.9 Costa Rica Earthquake
• Generally simple rupture– Simple source time function
– Fairly concentrated moment release on fault plane
– Some evidence for minor rupture directivity to SE
• Short rupture duration
1990
1999
1983
Rupture area ~600 km2
seamounts ~300-350 km2
Rupture area ~350 km2
Subducting features ~300-350 km2
Rupture area ~3000 km2
Ruptured lateral extent of Cocos Ridge
Locations of Highest Quality Events
DeShon et al., in review
Aftershock locations concentrate near regions of moment release
Significant diversity in focal mechanism of aftershocks
Summary
• Variable rupture processes observed for shallow seismogenic zone earthquakes in Costa Rica
• Comparison with detailed bathymetry suggests heterogeneous Cocos Plate topography influences large earthquake rupture