Allison K. Thurmond

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Key Points: • Strain in the lower crust is diffuse, while upper crustal strain is localized • The Red Sea rift axis likely migrated eastward gradually since the late Miocene • The lower crust beneath the Red Sea rift is decoupled from the upper crust (2014), Receiver function constraints on crustal seismic velocities and partial melting beneath the Red Sea(More)
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