Elimination approach:
2:1 clay minerals have two tetrahedral sheets sandwiching one octahedral sheet, giving them high shrink-swell capacity. Montmorillonite and Vermiculite are both classic 2:1 minerals, so they are ruled out. Halloysite is essentially a hydrated, tubular form of kaolinite but is far less abundant in soils. That leaves Kaolinite, a 1:1 mineral (one tetrahedral + one octahedral sheet held by hydrogen bonding, low shrink-swell, low CEC) as the most widespread 1:1 clay in weathered, tropical and sub-tropical soils.