Which mechanism drives the formation of elongated basins along oceanic transform faults?

💡 Explanation

When transform faults slip, strike-slip movement causes localized crustal thinning due to extensional forces along bends on the fault line, leading to basin formation because the lithosphere stretches and subsides. Therefore strike-slip induced crustal thinning is responsible, rather than the alternatives involving thermal, sedimentary accretion, or mantle upwelling which require different heat source or fault dynamics.

• During strong El Niño phases, which mechanism increases nutrient stratification influencing marine ecosystems off Peru?
• Which mechanism explains why major global deserts often appear ~30° latitude from the equator?
• Which geomorphic consequence results when a river's sinuosity increases significantly near an oxbow lake formation?
• Which effect arises from the deflection of prevailing winds by the Coriolis force?
• Which outcome occurs when accumulated sediment compacts during subduction?
• Upriver sediment load decrease causes increased channel sinuosity, producing which feature?