Seismic imaging and thermal modeling of active continental rifting processes in the Salton Trough, Southern California
Continental rifting ultimately creates a deep accommodation space for sediment. When a major river flows into a late-stage rift, thick deltaic sediment can change the thermal regime and alter the mechanisms of extension and continental breakup. The Salton Trough, the northernmost rift segment of the...
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Virginia Tech
2017
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| Online Access: | http://hdl.handle.net/10919/78906 |