Abstract
The Lower Ordovician Dumugol Formation in the southern part of the Baegunsan Syncline, Korea, comprises a succession of mixed siliciclastic and carbonate sediments. The depositional system of the Dumugol Formation is interpreted as a homoclinal ramp frequently influenced by storm activity, based on the lithological characteristics. Lithofacies associations are grouped into four depositional facies: shallow siliciclastic ramp, shallow carbonate ramp, deep carbonate ramp, and basin.
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