02348oam 2200457zu 450 99621475590331620210807004632.01-118-66691-7(CKB)3450000000004226(SSID)ssj0000815298(PQKBManifestationID)11512506(PQKBTitleCode)TC0000815298(PQKBWorkID)10807448(PQKB)11381191(NjHacI)993450000000004226(PPN)189561076(EXLCZ)99345000000000422620160829d1989 uy engur|||||||||||txtccrSouthern Appalachian Windows: Comparison of Styles, Scales, Geometry, and Detachment Levels of Thrust Faults in the Foreland and Internides of a Thrust-Dominated Orogen[Place of publication not identified]American Geophysical Union19891 online resource (ix, 93 pages) illustrationsField trip guidebook (International Geological Congress (28th : 1989 : Washington, D.C.)) ;T167Bibliographic Level Mode of Issuance: Monograph0-87590-616-8 Published by the American Geophysical Union as part of the Field Trip Guidebooks Series, Volume 167. The southern Appalachian orogen contains most of the subdivisions that characterize a classic collisional orogen: A foreland fold-and-thrust belt (Cumberland Plateau and Valley and Ridge), high-grade metamorphic core (central to eastern Blue Ridge and western Piedmont), and a plutonic/volcanic belt (Charlotte belt and Carolina slate belt). In addition, a younger Alleghanian high-grade metamorphic core is present on the eastern edge of the Piedmont (Kiokee-Raleigh belt).Field trip guidebook (International Geological Congress (28th : 1989 : Washington, D.C.)) ;T167.GeologyAppalachian Region, SouthernGuidebooksGeology557.688Hatcher Robert D.1429914HatcherPQKBBOOK996214755903316Southern Appalachian Windows: Comparison of Styles, Scales, Geometry, and Detachment Levels of Thrust Faults in the Foreland and Internides of a Thrust-Dominated Orogen3569532UNISA