Abstract

Current work funded by the Gas Research Institute indicates that, in Kanawha and Boone Counties, West Virginia, most gas wells completed in the Devonian shales produce from the lower part of the Upper Devonian Huron Member of the Ohio Shale. Discrete assemblages of black shale emplacement in this part of the Appalachian basin can be discerned and are mappable using log data from wells that penetrate the lower Huron section. Black shale isolith maps across the two-county area show discrete elongate trends of black shale, thinning predominantly from northeast to southwest. These elongate black shale minima are interpreted herein as sites where newly deposited, black organic mud substrates were scoured by the action of relatively high-velocity turbidite plumes entering this part of the basin from shallower regions toward the east and northeast. Turbidite-transported muds and silts were then laid in the newly scoured areas in close vertical and lateral contact with the surrounding black muds. This interfingering of organic black shales with the gray silty shales and siltstones is significant to gas production from the Devonian shales in that the interbedded nature of these rocks provides a mechanism whereby gas generated and held by absorption in the black shales canmore » migrate into the more porous and permeable gray shales and siltstones, hence from there into a fracture system or a well bore.« less

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