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Berea Sandstone
Method of evaluating cement-to-formation bond strength with computed tomography image analysis
Effective medium modeling of the joint elastic-electrical properties of sandstones with partial water saturation
A comparison of three-dimensional–printed porous rocks with nano x-ray computed tomography: Silica sand, gypsum powder, and resin
Estimation of transversely isotropic formation parameters using flexural and quadrupole dispersion data in the fast formation
Understanding how overpressure affects the physical properties of sandstones
Numerical modeling of multifrequency complex dielectric permittivity dispersion of sedimentary rocks
Berea Sandstone: New developments in a mature oil and gas play, eastern Kentucky and Ohio
Molecular and isotopic gas composition of the Devonian Berea Sandstone and implications for gas evolution, eastern Kentucky
Organic geochemistry and petrology of Devonian shale in eastern Ohio: Implications for petroleum systems assessment
Organic petrology and geochemistry of the Sunbury and Ohio Shales in eastern Kentucky and southeastern Ohio
Reservoir geology of the Berea Sandstone (uppermost Devonian), eastern Kentucky
Oil–source correlation studies in the shallow Berea Sandstone petroleum system, eastern Kentucky
V P and V S prediction from digital rock images using a combination of U-Net and convolutional neural networks
Berea sandstone: A heritage stone of international significance from Ohio, USA
Abstract Berea sandstone, a potential Global Heritage Stone Resource, has been one of the most widely used sandstones in North America. This Paleozoic sandstone, quarried for more than 200 years in Ohio, has been used across much of the continent. Thousands of commercial, residential, ecclesiastical, government and other structures have been built with Berea sandstone, including Thomas Worthington's mansion in Chillicothe, Ohio, the Michigan Capitol in Lansing, Michigan, the Carnegie Library and Natural History Museum Building in Pittsburgh, Pennsylvania, and parts of the Parliament buildings in Canada. Grindstones made from Berea sandstone were shipped throughout North America, as well as to the Caribbean, South America, Europe and Asia. The stone is celebrated in a number of locations, notably Berea and Amherst, where quarries have been important historical sources of this stone. It has been known by a number of different geological and commercial names, including Berea grit and Amherst stone, complicating its identification from historical sources. Stone from the most productive quarries, however, was known to be homogeneous and can be identified by its quartz–arenite to sublithic–arenite composition, its fine to medium sand (125–350 µm) grain size and iron-cement spots. Berea sandstone continues to be quarried today in Erie and Lorain counties.