Preservation of deposits resulting from instantaneous events preserved within sedimentary layers is the basis for correlation in

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Preservation of deposits resulting from instantaneous events is the basis for event stratigraphy. Biostratigraphy involves the use of fossil organisms to correlate sedimentary layers, while isotope stratigraphy utilizes variations in the ratios of isotopes to date and correlate layers. Lithostratigraphy correlates layers based on their lithologic properties.

Preservation of Deposits Resulting from Instantaneous Events Preserved Within Sedimentary