12.07.2015 Views

Ambientes Marinos Someros Clásticos

Ambientes Marinos Someros Clásticos

Ambientes Marinos Someros Clásticos

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Forma de depósitoFig2. Influencia de las mareas en océanos epicontinentales.Dependerá de la velocidad de corriente• Baja velocidad(50 cm s^‐1) Sábanas de bajo relieve

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