Electronic Supplement to
Relocated Hypocenters and Structural Analysis from Waveform Modeling of Aftershocks from the 2011 Prague, Oklahoma, Earthquake Sequence

by Marius P. Isken and Walter D. Mooney

Table S2. Normally Distributed Constraints of the Modeled Paleochannels

Channel Property	Value	Description
Channel width	200–700 m	Width of the paleochannel
Channel maximum depth	50–400 m	Maximal vertical extent of the paleochannel
Skewness of channel	0.3–0.4	Trigonometric skewness of the channel riverbed
Relative velocity contrast	90%–60%	Relative velocity contrast to the embedding limestone gradient layer

The dimensions of the channels are learnt from investigations by Joseph (1986).

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