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- W1679210005 abstract "In 2004 tomographic results from the La Ristra array revealed a fast seismic velocity anomaly beneath the eastern flank of the Rio Grande rift. The location and geometry of the anomaly led to the hypothesis that it was the result of edge-driven convection. The linear array imaged the anomaly in only two dimensions, however, warranting further three-dimensional modeling. To investigate the hypothesis, a twodimensional array was deployed through the Seismic Investigation of Edge-Driven Convection Associated with the Rio Grande Rift (SIEDCAR) project." @default.
- W1679210005 created "2016-06-24" @default.
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- W1679210005 date "2010-12-01" @default.
- W1679210005 modified "2023-09-28" @default.
- W1679210005 title "Seismic Tomographic Imaging of an Upper Mantle Anomaly beneath the Rio Grande Rift" @default.
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