SYSTEMATIC NON-DOUBLE-COUPLE COMPONENTS OF EARTHQUAKE MECHANISMS - THE ROLE OF FAULT ZONE IRREGULARITY

Authors
Citation
K. Kuge et T. Lay, SYSTEMATIC NON-DOUBLE-COUPLE COMPONENTS OF EARTHQUAKE MECHANISMS - THE ROLE OF FAULT ZONE IRREGULARITY, J GEO R-SOL, 99(B8), 1994, pp. 15457-15467
Citations number
31
Categorie Soggetti
Geosciences, Interdisciplinary
Journal title
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
ISSN journal
21699313 → ACNP
Volume
99
Issue
B8
Year of publication
1994
Pages
15457 - 15467
Database
ISI
SICI code
2169-9313(1994)99:B8<15457:SNCOEM>2.0.ZU;2-#
Abstract
Several recent studies have revealed statistical correlations between earthquake mechanism type and associated non-double-couple components in catalogs of seismic moment tensors. This systematic behavior may re sult either from biases in the solutions due to Earth structure effect s in different tectonic regimes, or from source radiation effects. For certain large non-double-couple events, detailed analyses have shown that multiple subevents with different fault orientations produce the non-double-couple radiation. We generalize this idea and simulate non- double-couple components (NDCC) resulting from subfaults with variable geometry, showing that the statistical behavior of the NDCC in moment tensor catalogs can be generally accounted for by such source complex ity. Assuming that an earthquake fault consists of many subfaults with random fluctuations about some mean geometry, the total moment tensor for failure of the system under a regional stress state can be repres ented by the sum of moment tensors of the subfaults. The sign of the N DCC in the composite moment tensor directly reflects the stress state applied to the fault system, and the NDCC amplitude is expected to be systematic over a wide range of cumulative seismic moment (M(o)) given the basic fractal nature of fault systems. These simulation results a re consistent with the global behavior of the NDCC reported in the Har vard centroid moment tensor catalog for 1977-1991. Parameters such as the applied stress state, parameterization and randomness of the subfa ult geometry, and seismic moment distribution among the subfaults affe ct the predicted NDCC amplitude. Change in the parameters as a functio n of subfault seismic moment controls the shape of the NDCC - M(o) rel ationship. Regional variations of the NDCC - M(o) relationship may thu s reflect regional variations in the fault zone parameters, raising th e possibility that the regional NDCC behavior may be used to infer str ess state and subfault distribution in various source regions.