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• W2073077181 abstract "Widespread observations of crustal reflections in conjunction with delayed refracted phases have been interpreted as evidence of upper crustal low-velocity layers. A plausible explanation of the low-velocity effect, determined from laboratory experiments on granites, suggests a decrease in the P-wave velocity of up to 0.2 km/sec in the depth range of 6–15 km that is produced by high temperatures. Synthetic seismograms computed for velocity-depth functions calculated from these temperature effects and corresponding to regional heat-flow provinces indicate three characteristics that define the upper crustal low-velocity layer: (1) high attenuation of Pg, (2) the presence of wide-angle, large-amplitude reflections (PcR), and (3) large PcR-Pg time differences. As an example of the possible effects of high heat flow (∼2.5 HFU), an upper crustal low-velocity layer is shown to correlate with a thin crust (25 km), a 9-km mantle upward, Pn velocities as low as 7.5 km/sec, an area of active seismicity, and a Cenozoic zone of normal faulting that all occur along the Basin Range-Colorado Plateau transition zone of the western United States." @default.
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• W2073077181 date "1975-12-01" @default.
• W2073077181 modified "2023-09-25" @default.
• W2073077181 title "Upper crustal low-velocity layers: Possible effect of high temperatures over a mantle upwarp at the basin range-Colorado plateau transition" @default.
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• W2073077181 doi "https://doi.org/10.1016/0012-821x(75)90227-7" @default.
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