LEADER 02348oam 2200457zu 450 001 996214755903316 005 20210807004632.0 010 $a1-118-66691-7 035 $a(CKB)3450000000004226 035 $a(SSID)ssj0000815298 035 $a(PQKBManifestationID)11512506 035 $a(PQKBTitleCode)TC0000815298 035 $a(PQKBWorkID)10807448 035 $a(PQKB)11381191 035 $a(NjHacI)993450000000004226 035 $a(PPN)189561076 035 $a(EXLCZ)993450000000004226 100 $a20160829d1989 uy 101 0 $aeng 135 $aur||||||||||| 181 $ctxt 182 $cc 183 $acr 200 00$aSouthern Appalachian Windows: Comparison of Styles, Scales, Geometry, and Detachment Levels of Thrust Faults in the Foreland and Internides of a Thrust-Dominated Orogen 210 31$a[Place of publication not identified]$cAmerican Geophysical Union$d1989 215 $a1 online resource (ix, 93 pages) $cillustrations 225 1 $aField trip guidebook (International Geological Congress (28th : 1989 : Washington, D.C.)) ;$vT167 300 $aBibliographic Level Mode of Issuance: Monograph 311 $a0-87590-616-8 330 $aPublished by the American Geophysical Union as part of the Field Trip Guidebooks Series, Volume 167. The southern Appalachian orogen contains most of the subdivisions that characterize a classic collisional orogen: A foreland fold-and-thrust belt (Cumberland Plateau and Valley and Ridge), high-grade metamorphic core (central to eastern Blue Ridge and western Piedmont), and a plutonic/volcanic belt (Charlotte belt and Carolina slate belt). In addition, a younger Alleghanian high-grade metamorphic core is present on the eastern edge of the Piedmont (Kiokee-Raleigh belt). 410 0$aField trip guidebook (International Geological Congress (28th : 1989 : Washington, D.C.)) ;$vT167. 606 $aGeology$zAppalachian Region, Southern$vGuidebooks 615 0$aGeology 676 $a557.688 700 $aHatcher$b Robert D.$01429914 702 $aHatcher 801 0$bPQKB 906 $aBOOK 912 $a996214755903316 996 $aSouthern Appalachian Windows: Comparison of Styles, Scales, Geometry, and Detachment Levels of Thrust Faults in the Foreland and Internides of a Thrust-Dominated Orogen$93569532 997 $aUNISA