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The AAPG/Datapages Combined Publications Database

Ohio Geological Society

Abstract

OGS-AAPG

Ohio Geological Society: The New Clinton Collection, , 1985

Pages 233 - 242

THE SILURIAN BRASSFIELD-ROCHESTER SHALE SEQUENCE IN THE SUBSURFACE OF EASTERN OHIO

Bradford E. Nelson, Canton Oil Well Service, Inc., 5940 Mayfair Road N.W., North Canton, Ohio 44720
Alan H. Coogan, Department of Geology, Kent State University, Kent, Ohio 44242

ABSTRACT

The Early-Middle Silurian Brassfield-Packer Shell-Rochester Shale interval in the subsurface of eastern Ohio thickens ten-fold 'from west to east and southeast toward the clastic source area. The carbonate units in the interval also thicken six-fold. The subsurface carbonate units, the Packer Shell limestone, Casing Shell limestone and unnamed carbonate rock units axe the equivalent of the Brassfield Limestone of the outcrop in southern Ohio. The Brassfield splits in the subsurface into many carbonate rock units which are interbedded with the Rochester Shale. The base of the Brassfield-Packer Shell is a disconformable surface. The basal carbonate unit of the interval onlaps the underlying clastic deposits of the Clinton sandstone interval (Medina Group of New York). The lower surface is a satisfactory marker horizon for subregional correlation and structural mapping. The whole interval between the Clinton sandstone and the Lockport (Niagaran) Group dolomites is time-transgressive from west to east.

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