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The subsurface uncertainty at West Virginia University Main Campus is dominated by the uncertainty in the projections of geofluid flowrate in the target formation, the Tuscarora Sandstone. In this paper, three cores from the heterogeneous reservoir, available through West Virginia Geologic and Economic Survey, are analyzed by performing core analysis using CT scanning and permeability measurements via minipermeameter. Additional geological data are collected through cores, published literature, seismic data, and nearby, existing wells to estimate thickness, fracture network configuration and geothermal gradient to minimize the uncertainty of well deliverability. Using these estimated reservoir properties; a 3D conceptual model for the proposed geothermal site is developed. This dataset includes a GRC conference publication along with the data used to produce results explained in the paper including minipermeability measurement data for Preston -119 core and thin section analysis photos and data for Clay-513 core.

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Format	Description	Link
33	Conference Paper	https://gdr.openei.org/files/1097/GRC_2018_RevisiedPaper_WVU.pdf
36	Conference Presentation	https://gdr.openei.org/files/1097/GRC2018_DDU_WVU.pptx
36	Clay-513 Thin Section analysis Picutres	https://gdr.openei.org/files/1097/Clay_513%20Thin%20Section%20Photos_RMcDowell.pptx
53	Clay-513 Thin Section analysis Observations	https://gdr.openei.org/files/1097/Clay_513_ThinSection_Desc_RMcDowell.xlsx
53	Preston-119 Mini permeability measurement data	https://gdr.openei.org/files/1097/Preston-119_FINAL_core_permeability_illustrated.xlsx

Development of 3D Geological Model of Tuscarora Sandstone for Feasibility of Deep Direct-Use Geothermal at West Virginia University Main Campus

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