dc.rights.license | In Copyright | en_US |
dc.creator | Dunlevy, Colleen Alayne | |
dc.date.accessioned | 2023-10-20T17:40:18Z | |
dc.date.available | 2023-10-20T17:40:18Z | |
dc.date.created | 1996 | |
dc.identifier | WLURG038_Dunlevy_thesis_1996 | |
dc.identifier.uri | https://dspace.wlu.edu/handle/11021/36356 | |
dc.description.abstract | The 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.extent | 40 pages | en_US |
dc.language.iso | en_US | en_US |
dc.rights | This 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.uri | http://rightsstatements.org/vocab/InC/1.0/ | en_US |
dc.title | Sedimentology and Depositional Setting of the Miocene Marnoso-Arenacea Flysch, Marche region, Italy | en_US |
dc.type | Text | en_US |
dcterms.isPartOf | WLURG038 - Student Papers | en_US |
dc.rights.holder | Dunlevy, Colleen Alayne | en_US |
dc.subject.fast | Geology -- Italy | en_US |
dc.subject.fast | Sedimentation and deposition -- Italy | en_US |
dc.subject.fast | Sediments (Geology) -- Italy | en_US |
dc.subject.fast | Miocene Geologic Epoch -- Italy | en_US |
dc.subject.fast | Flysch -- Italy | en_US |