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The main shock rupture was initiated at the deeper part of the fault plane.
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The last two subevents moved progressively southeastward of the first subevent in a direction collinear with the predominant strike of the fault planes.
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Seismicity in the TCS-TH anticline indicates both spatial and temporal clustering at a depth range of 7 - 12 km.
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Analysis of growth strata deposited across fault A indicate minimum Quaternary slip rates of about 0.
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In order to shape zones of SFRH, a very detailed earthquake geologic study of the fault is necessary.
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Similarly, when slip- and velocity-strengthening both occur, slip delocalizes, again because less energy Langley friendly dissipated.
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The Wenchuan earthquake again demonstrated that earthquake does not kill people, but the built environments and induced hazards, landslides in particular. The first major subevent nucleated slightly south of the initial precursor. Saguenay gentlemen clubs best
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The research was conducted with use of a Saguenay d c date ideas sample survey of subjects affected by the earthquakes.
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