Which mechanism causes sediment accumulation in pull-apart basins along strike-slip faults?

💡 Explanation

When strike-slip movement occurs along transform faults, pull-apart basins form because localized crustal extension induces thinning and subsidence, creating topographic lows that trap sediment. Therefore sag basins forming results, rather than reverse drag, tilted blocks, or horst-graben structures which arise from different tectonic compressional regimes.

• Which consequence results when coastal upwelling ceases near a major fishing ground?
• Which mechanism causes the Intertropical Convergence Zone to experience a seasonal shift in latitude?
• Which mechanism causes thermohaline circulation within a large endorheic lake basin experiencing rapid evaporation?
• Which outcome occurs when tectonic activity interrupts thermohaline circulation?
• Which process limits the average depth of fjords subjected to glacial rebound?
• Which mechanism alters surface salinity within subtropical gyres located far from landmasses?