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

💡 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.

• Which geologic outcome occurs when a transform fault offsets a mid-ocean ridge?
• Which ground surface instability event increases as permafrost thaws?
• Which deposition pattern emerges when stream confinement suddenly ends?
• Which outcome results due to intensified physical weathering during pedogenesis?
• Which effect accelerates downslope movement via solifluction in high-latitude permafrost regions?
• Which process primarily initiates cirque formation in mountainous glacial regions?