Which outcome is favored along strike-slip faults exhibiting geometric complexity?

💡 Explanation

Localized compressional zones develop because geometric complexities, like bends in strike-slip faults, generate transpression; therefore, localized compression results, rather than broad extension due to divergence or uniform slip as fault locks up.

• Which consequence results when strike-slip transform boundaries lock?
• Which mechanism initially prevents continued displacement along an established strike-slip fault line?
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• Which effect occurs when extensive grassland is overgrazed within a loess deposit region, exposed to seasonal wind?
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