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dc.creatorRoot, S. I.en_US
dc.creatorMacWilliams, R. H.en_US
dc.date.accessioned2006-07-07T02:19:40Z
dc.date.available2006-07-07T02:19:40Z
dc.date.issued1986-09en_US
dc.identifier.citationThe Ohio Journal of Science. v86, n4 (September, 1986), 161-163en_US
dc.identifier.issn0030-0950en_US
dc.identifier.urihttp://hdl.handle.net/1811/23152
dc.descriptionAuthor Institution: Department of Geology, The College of Woosteren_US
dc.description.abstractA ground-derived total intensity magnetic map of the Suffield fault, a western extension of the Transylvania fault zone, suggests a fault with a southwest dip of 80° or greater. Displacement history is uncertain, but may involve significant right-lateral wrenching at the time of early fault development. Subsequent movements may include normal faulting. Although principal fault movement is Permo- Pennsylvanian, displacement at the level of the Precambrian surface, inferred from the magnetic map, suggests significant Cambro-Ordovician faulting. Subsurface distribution patterns of Silurian to Mississippian units define minor syndepositional fault movements during accumulation of the Silurian Salina salts and again during deposition of the Mississippian Berea sands.en_US
dc.format.extent343220 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.titleThe Suffield Fault, Stark County, Ohioen_US


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