10 de maio de 2010

Princípio da Continuidade Lateral

Em colunas estratigráficas de dois lugares afastados é possível relacionar cronologicamente estratos idênticos dos dois locais (mesmo que tenham dimensões variáveis), desde que as sequências de deposição sejam semelhantes.

Reflexão: Assim, se as rochas estiverem intercaladas em rochas idênticas, mesmo que estejam distantes, pode estabelecer-se uma correlação de idade, ajudando-nos na datação de estratos.

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