What type of pressure-temperature pathway represents subduction zone metamorphism?

Name: What type of pressure-temperature pathway represents subduction zone metamorphism?
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Subduction zone metamorphism occurs at high pressures and relatively low temperatures as a result of the descending of cold oceanic lithosphere underneath the overriding plate. This creates a high-pressure, low-temperature environment conducive to the formation of minerals like blueschist, eclogite, and garnet.

What Type of Pressure-Temperature Pathway Represents Subduction Zone Metamorphism