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Tibetan Plateau Crust and Mantle Structure Down to 700 km Depth as Derived From Seismological Data (Invited)
Tibetan Plateau Crust and Mantle Structure Down to 700 km Depth as Derived From Seismological Data (Invited)
2010
James Mechie
R. Kind
Joachim Saul
Keywords:
Crust
Mesosphere (mantle)
Receiver function
Oceanic crust
Mantle (geology)
Low-velocity zone
Geophysics
Geology
Transition zone
Plateau
Correction
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