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- W1815094002 abstract "Over the past decades, the seismic structure of the crust and upper mantle of the southwestern United States was examined using an array of different methods. The structure and composition of crust received special attentions, most due to the hydrocarbon reserves in this area. Here new constraints on crustal evolution and structure models are provide by systematically analyzing 37,402 receiver functions recorded at 234 seismic stations on the southwestern United States. The results reveal that the Transitional Crust is characterized by a thin (29.0±1.0 km) crust, a low Vp/Vs ratio of 1.76±0.016 and a high amplitude (R) of P-to-S converted waves (relative to that of the direct P wave) of 0.258±0.028, consistent with the model that the thin crust was the consequence of lithospheric stretching during the opening of the Gulf of Mexico and that this area is covered by a thick sedimentary layer. The Precambrian Grenville and Yavapai Provinces are characterized by a thick crust (41.8±0.7 km), large Vp/Vs (1.791±0.030) and smalle R (0.156±0.019) values, indicating that this area experienced no significant stretching. The Rio Grande Rift Area has a thin crust (35.6±0.8 km) and an intermediate Vp/Vs (1.78±0.025) ratio that is similar to a typical continental crust, and a large R value (0.216±0.033), suggesting that the crustal thinning was the result of pure shear stretching." @default.
- W1815094002 created "2016-06-24" @default.
- W1815094002 creator A5070982537 @default.
- W1815094002 date "2014-01-01" @default.
- W1815094002 modified "2023-09-27" @default.
- W1815094002 title "A receiver function study of crust thickness and composition beneath the southwestern United States" @default.
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