Petrogenesis, P-T-t path, and tectonic significance of high-pressure mafic granulites from the Jiaobei terrane, North China Craton

- The inherited metamorphic cores and retrogressive rims can be identified in single zircon grains.
- Retrogressive metamorphic mineral inclusions have been identified in zircon grains.
- A near-isothermal decompressional clockwise P-T-t path for the Jiaobei HP mafic granulites is defined.