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• W2092026483 abstract "The lithospheric structure beneath the Colorado Plateau and Great Basin of the western United States is investigated using Pn and surface wave data from the Colorado Plateau ‐ Great Basin broadband seismic experiment. Average Pn velocities of 8.0 km/s in the Colorado Plateau and 7.8 km/s in the eastern Great Basin are found. Teleseismic Rayleigh waves are also measured, and eastern Great Basin phase velocities are found to be 3–4% higher than Colorado Plateau phase velocities in the 20–35 s range, but indistinguishable at periods greater than 40 s. The apparent Pn/surface wave discrepancy is resolved with models that include a thicker crust and faster mantle lid for the Colorado Plateau than the eastern Great Basin. Models for both regions require a mantle low velocity zone. The slow mantle deep beneath the Colorado Plateau may suggest a thermal origin of Plateau uplift, which has not yet penetrated the mantle lid." @default.
• W2092026483 created "2016-06-24" @default.
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• W2092026483 date "2001-04-01" @default.
• W2092026483 modified "2023-09-27" @default.
• W2092026483 title "Seismic evidence for partial lithospheric delamination model of Colorado Plateau Uplifts" @default.
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• W2092026483 doi "https://doi.org/10.1029/2000gl012360" @default.
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