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dc.creatorDean, Stuart L.en_US
dc.creatorKulander, Byron R.en_US
dc.creatorForsyth, Jane L.en_US
dc.creatorTipton, Ronald M.en_US
dc.date.accessioned2006-07-07T17:57:21Z
dc.date.available2006-07-07T17:57:21Z
dc.date.issued1991-03en_US
dc.identifier.citationThe Ohio Journal of Science. v91, n1 (March, 1991), 2-15en_US
dc.identifier.issn0030-0950en_US
dc.identifier.urihttp://hdl.handle.net/1811/23425
dc.descriptionAuthor Institution: Department of Geology, University of Toledo, Department of Geological Sciences, Wright State University, Department of Geology, Bowling Green State University and France Stone Companyen_US
dc.description.abstractBedrock in northern and northwestern Ohio consists of Middle Paleozoic carbonates and shales and is pervasively jointed. The regional joint pattern and chronology, established by the characteristics of joint traces, mineralization, and surfaces, reveal a complex history of fracture development. Joint studies along the north-south trending Bowling Green fault zone indicate that northwest-trending joints formed first in response to extensional stresses associated with differential dip-slip movement in this fault zone, or by left lateral movement along this zone.en_US
dc.format.extent5829492 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.titleField Guide to Joint Patterns and Geomorphological Features of Northern Ohioen_US


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