BASAL SAUK SEQUENCE IN THE SUBSURFACE OF OHIO-- MT. SIMON SANDSTONE
The MSS disconformably overlies the Precambrian Middle Run Formation. The contact is readily apparent in cores as a transition from the dark reddish brown, highly indurated and well cemented, poorly sorted, angular, fine- to medium-grained lithic arenite and quartz-feldspar-rhyolite-quartzite-chert pebble conglomerate of the Middle Run Formation to the tan, friable, moderately sorted, rounded, coarse- to very coarse-grained siliceous quartz arenite and quartz granule conglomerate of the MSS. Gamma-ray and neutron-porosity logs notably decrease across the contact.
The MSS contains tidal rhythmites, lenticular-, flaser-, and wavy-bedding, herringbone cross-bedding, mud-drapes, tidal bundles, reactivation surfaces, intraclasts, and bioturbation. The unit generally coarsens and thickens upwards. The MSS is interpreted as a transgressive barrier sequence in which the barrier (the bulk of the MSS) migrated across a basal estuarine/lagoonal sequence. The upper progradational, shoaling- and fining-upward parts of the MSS observed in Wisconsin and the Michigan Basin are absent in western Ohio. Instead, the MSS is conformably overlain by tidal flat and off-shore deposits of the Eau Claire Formation.
The Eau Claire Formation is readily recognized in cores as the transition to gray, fine-grained, feldspathic arenite and shale, typically intensely bioturbated and mottled, with marine macrofossils. The geophysical signature of the contact is a pronounced increase in gamma-ray and neutron-porosity logs.