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dc.rights.licenseIn Copyrighten_US
dc.creatorDunlevy, Colleen Alayne
dc.date.accessioned2023-10-20T17:40:18Z
dc.date.available2023-10-20T17:40:18Z
dc.date.created1996
dc.identifierWLURG038_Dunlevy_thesis_1996
dc.identifier.urihttps://dspace.wlu.edu/handle/11021/36356
dc.description.abstractThe Coldigioco-Castellaro basin is the Easternmost basin in a series of basins and adjacent topographic highs formed during the Early Miocene epoch by compression that produced the Italian Northern Apennines. Part of the Marnoso-Arenacea flysch, a sequence of sandstone, conglomerate, and mudstone, accumulated in this late stage basin bounded by two, synsedimentary, thrust-produced anticlines. This study examines the influence of the anticlines on flysch sedimentation in the basin.en_US
dc.format.extent40 pagesen_US
dc.language.isoen_USen_US
dc.rightsThis material is made available for use in research, teaching, and private study, pursuant to U.S. Copyright law. The user assumes full responsibility for any use of the materials, including but not limited to, infringement of copyright and publication rights of reproduced materials. Any materials used should be fully credited with the source.en_US
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/en_US
dc.titleSedimentology and Depositional Setting of the Miocene Marnoso-Arenacea Flysch, Marche region, Italyen_US
dc.typeTexten_US
dcterms.isPartOfWLURG038 - Student Papersen_US
dc.rights.holderDunlevy, Colleen Alayneen_US
dc.subject.fastGeology -- Italyen_US
dc.subject.fastSedimentation and deposition -- Italyen_US
dc.subject.fastSediments (Geology) -- Italyen_US
dc.subject.fastMiocene Geologic Epoch -- Italyen_US
dc.subject.fastFlysch -- Italyen_US


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