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1. MARCO GEOLOGICO Y GEODINAMICO GENERAL DEL ÁREA DEL AEROPUERTO . La Depresión Interandina es una estructura extensional importante limitada por escarpes de fallas activas y parcialmente rellenadas por depósitos continentales y volcano-sedimentarios que localmente alcanzan un espesor de algunos miles de metros (Baldock, 1985) a y se cree que casi reflejan la joven historia … ................
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