Strong earthquakes often occur in regions that are located between upheaval and subsidence of the Moho surface or density reduction and density increase of the interface.
地震往往发生在莫霍面隆起区与沉降区、密度减小区与增长区的过渡地带。
Strong earthquakes often occur in regions that are located between upheaval and subsidence of the Moho surface or density reduction and density increase of the interface.
地震往往发生在莫霍面隆起区与沉降区、密度减小区与增长区的过渡地带。
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