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Although continental crust has a different composition from that of oceanic crust, the boundary between the two crustal types may not be clearly defined; sometimes gradational or oceanic crust may even intrude into extended and downthrown continental crust.
Aunque la corteza continental y la corteza oceánica no tienen la misma composición, puede no estar clara la línea de demarcación entre ambos tipos de corteza, en ocasiones la corteza gradacional y la corteza oceánica se superponen o se imbrican en la corteza continental.
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