The crustal structure of Beira High, central Mozambique—Combined investigation of wide-angle seismic and potential field data
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文摘

Beira High is composed of stretched, but highly intruded continental crust.

Narrow continent-ocean transition is located at the south-eastern end of Beira High.

Crust below the Zambezi Delta Depression is thin and underplated.

Amplitude modelling and density gradient model support the wide-angle seismic study.

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