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Geography

Which outcome is promoted at strike-slip faults crossing shallow geothermal reservoirs?

A)Higher permeability fracture networks
B)Diminished convective heat flux
C)Increased mineral deposition rates
D)Enhanced sediment accumulation rates

💡 Explanation

Higher permeability fracture networks develop due to the repeated displacement along faults; this process, known as fault gouge formation, increases the interconnectedness of pores. Therefore, geothermal flow is maintained, rather than heat flux decreasing because blocked pathways prevent fluid motion.

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