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Yellow dots: upper half of the surrounding damage zones (sdz).
Low GSI values were seen to outline tectonic damage zones.
Damage zones on the specimens were also examined in detail.
Thus, damage zones of large-scale fault zones are prime targets for geothermal exploration.
These areas correspond to the surrounding damage zones (Figures 2 and 10).
Areas outside the surrounding damage zones and brecciated zones are named the intact zones.
The average half width of the studied damage zones ranges between 12 and 14.5 m.
These faults are dominated by mixed zones with poorly developed fault cores and damage zones.
However, constant size and regular shape of damage zones cannot be obtained by recent RFA technologies.
Various recommended blasting damage zones are considered, and disturbance factors are used to represent damage levels.
Joints and water were found to significantly affect the damage zones.
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