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fault plane
This term is a specialized geological descriptor used primarily in seismology and structural geology. It describes the specific geometric surface of a rupture, distinguishing the actual plane of movement from the general area of a fault zone. It is used in technical reports and academic papers to describe the orientation, dip, and strike of a seismic event.
Because it refers to a specific physical boundary within the Earth's crust, it is used in a literal, scientific sense. It is rarely used metaphorically. In professional discourse, it is often paired with terms like "slip" or "displacement" to describe the kinematics of an earthquake.