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Field Guide to Joint Patterns and Geomorphological Features of Northern Ohio

Please use this identifier to cite or link to this item: http://hdl.handle.net/1811/23425

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dc.creator Dean, Stuart L. en_US
dc.creator Kulander, Byron R. en_US
dc.creator Forsyth, Jane L. en_US
dc.creator Tipton, Ronald M. en_US
dc.date.accessioned 2006-07-07T17:57:21Z
dc.date.available 2006-07-07T17:57:21Z
dc.date.issued 1991-03 en_US
dc.identifier.citation The Ohio Journal of Science. v91, n1 (March, 1991), 2-15 en_US
dc.identifier.issn 0030-0950 en_US
dc.identifier.uri http://hdl.handle.net/1811/23425
dc.description Author Institution: Department of Geology, University of Toledo, Department of Geological Sciences, Wright State University, Department of Geology, Bowling Green State University and France Stone Company en_US
dc.description.abstract Bedrock 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.extent 5829492 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.title Field Guide to Joint Patterns and Geomorphological Features of Northern Ohio en_US