Lehmann discontinuity

E2199080 UNEXPLORED

The Lehmann discontinuity is a seismic boundary within the Earth's mantle marked by an abrupt change in the velocity of seismic waves, named after Danish seismologist Inge Lehmann.

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Label	Occurrences
Lehmann discontinuity canonical	1

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Inge Lehmann → eponymOf → Lehmann discontinuity ⓘ