Interacting Intraplate Fault Systems in Australia: The 2012 Thorpdale, Victoria, Seismic Sequences
Autor: | Mike Sandiford, L. S. Schleicher, Abraham Jones, Januka Attanayake, Gary Gibson, Dan Sandiford |
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Rok vydání: | 2019 |
Předmět: |
geography
geography.geographical_feature_category 010504 meteorology & atmospheric sciences Magnitude (mathematics) Slip (materials science) Fault (geology) Induced seismicity 01 natural sciences Stress field Geophysics Space and Planetary Science Geochemistry and Petrology Earth and Planetary Sciences (miscellaneous) Intraplate earthquake Thrust fault Seismology Aftershock Geology 0105 earth and related environmental sciences |
Zdroj: | Journal of Geophysical Research: Solid Earth |
ISSN: | 2169-9356 2169-9313 |
DOI: | 10.1029/2018jb016945 |
Popis: | Using a new seismic waveform data set, we locate 234 earthquakes and estimate source parameters (focal mechanisms, magnitude, and stress drop) of the two largest earthquakes (E1 and E2) in the 2012 seismic sequence in Thorpdale, Victoria. The focal mechanisms suggest thrust faulting, consistent with previous observations in southeast Australia. The estimated magnitudes are Mw 4.9 ± 0.14 (E1) and 4.3 ± 0.1 (E2). The estimates of stress drop 57 ± 7.4 MPa (E1) and 28 ± 2.4 MPa (E2) reflect strength of faults in an intraplate environment. By analyzing spatiotemporal distribution of aftershocks, we show that E1 and E2 reflect two separate seismic sequences about a month apart. E1 and E2 ruptured two adjacent faults with orientations 218°/78°/78° (Fault 1) and 134°/27°/171° (Fault 2), respectively, where angles indicate strike/dip/slip rake. To test causal mechanism of fault interaction, we performed Coulomb stress modeling, which shows very weak unloading of E2 by E1. Thus, we infer that fault interaction might instead reflect remotely triggered fluid diffusion. Also, a local rotation of the stress field proceeding E1 might have favorably reoriented Fault 2 for failure. Finally, we identify an apparent correlation between high heat flow and seismicity in southeastern Australia, suggesting a combination of mechanisms including transient stress perturbations and lithospheric thermal weakening associated with high heat flow as the principal factors localizing intraplate seismicity. |
Databáze: | OpenAIRE |
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