- Plume–LIP dynamics can influence both proximal and distal mineral systems.
- Proximal effects include stress change, basin tilting, fracture (radial and circumferential) development and thermal–magmatic input.
- These processes may affect magmatic sulphides, IOCG, and uranium and other sediment-hosted systems.
- Distal plume push can change plate-scale stress and motion, influencing orogenic gold and porphyry systems.
- Plume geometry and timing provide new predictive criteria for regional mineral exploration.




