LEADER 01318nam2-22004331i-450- 001 990003918510403321 005 20090504153047.0 010 $a88-7011-548-8 035 $a000391851 035 $aFED01000391851 035 $a(Aleph)000391851FED01 035 $a000391851 100 $a20030910d1993----km-y0itay50------ba 101 1 $aita$ceng 102 $aIT 105 $a--------001cy 200 1 $aCome ridurre le diseguaglianze mondiali$fUNPD$g[traduzione dall'inglese di Claudia Di Giorgio] 210 $aTorino$cRosemberg & Sellier$d1993 215 $a226 p.$ctab., graf.$d28 cm 454 0$12001$aHuman development report 1992$931803 461 0$1001000391302$aRapporto su Lo sviluppo umano$v3 517 1 $aRapporto 1992 su Lo sviluppo umano 610 0 $aDiseguaglianza$aAspetti sociali 676 $a306.3$v21$zita 676 $a303.44$v21$zita 676 $a338.91 710 02$aUnited Nations Development Programme$0118788 801 0$aIT$bUNINA$gRICA$2UNIMARC 901 $aBK 912 $a990003918510403321 952 $a306.3 UNDP 3$b1100$fBFS 952 $aM/2 RAP/3$b12825$fSES 952 $aVI D 167 (3)$fFSPBC 952 $aVI D 168 (3)$fFSPBC 959 $aBFS 959 $aSES 959 $aFSPBC 996 $aHuman development report 1992$931803 997 $aUNINA LEADER 03541nam 2200673Ia 450 001 9910456856403321 005 20200520144314.0 010 $a0-8147-3234-8 010 $a0-8147-3315-8 010 $a1-4416-3662-5 024 7 $a10.18574/9780814733158 035 $a(MiAaPQ)EBC865489 035 $a(OCoLC)779828098 035 $a(OCoLC)558991452 035 $a(MdBmJHUP)muse4859 035 $a(DE-B1597)547059 035 $a(DE-B1597)9780814733158 035 $a(Au-PeEL)EBL865489 035 $a(CaPaEBR)ebr10356701 035 $a(EXLCZ)992520000000007939 100 $a20090727d2010 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 10$aShow sold separately$b[electronic resource] $epromos, spoilers, and other media paratexts /$fJonathan Gray 210 $aNew York $cNew York University Press$d2010 215 $a1 online resource (260 p.) 300 $aDescription based upon print version of record. 311 $a0-8147-3195-3 311 $a0-8147-3194-5 320 $aIncludes bibliographical references and index. 327 $tFrontmatter -- $tContents -- $tAcknowledgments -- $tIntroduction -- $t1. From Spoilers to Spinoffs -- $tIndex -- $tAbout the Author 330 $aIt is virtually impossible to watch a movie or TV show without preconceived notions because of the hype that precedes them, while a host of media extensions guarantees them a life long past their air dates. An onslaught of information from print media, trailers, internet discussion, merchandising, podcasts, and guerilla marketing, we generally know something about upcoming movies and TV shows well before they are even released or aired. The extras, or ?paratexts,? that surround viewing experiences are far from peripheral, shaping our understanding of them and informing our decisions about what to watch or not watch and even how to watch before we even sit down for a show.Show Sold Separately gives critical attention to this ubiquitous but often overlooked phenomenon, examining paratexts like DVD bonus materials for The Lord of the Rings, spoilers for Lost, the opening credits of The Simpsons, Star Wars actions figures, press reviews for Friday Night Lights, the framing of Batman Begins, the videogame of The Thing, and the trailers for The Sweet Hereafter. Plucking these extra materials from the wings and giving them the spotlight they deserve, Jonathan Gray examines the world of film and television that exists before and after the show. 606 $aAdvertising$xTelevision programs$xSocial aspects 606 $aAdvertising$xMotion pictures$xSocial aspects 606 $aTelevision programs$xMarketing$xSocial aspects 606 $aMotion pictures$xMarketing$xSocial aspects 606 $aParatext 606 $aIntertextuality 606 $aMass media and culture 608 $aElectronic books. 615 0$aAdvertising$xTelevision programs$xSocial aspects. 615 0$aAdvertising$xMotion pictures$xSocial aspects. 615 0$aTelevision programs$xMarketing$xSocial aspects. 615 0$aMotion pictures$xMarketing$xSocial aspects. 615 0$aParatext. 615 0$aIntertextuality. 615 0$aMass media and culture. 676 $a659.1/9302234 700 $aGray$b Jonathan$g(Jonathan Alan)$0989808 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910456856403321 996 $aShow sold separately$92353293 997 $aUNINA LEADER 04005oam 2200589zu 450 001 9910830467103321 005 20210807004712.0 010 $a1-118-66739-5 035 $a(CKB)3450000000004138 035 $a(SSID)ssj0000904874 035 $a(PQKBManifestationID)11494234 035 $a(PQKBTitleCode)TC0000904874 035 $a(PQKBWorkID)10924121 035 $a(PQKB)10374937 035 $a(NjHacI)993450000000004138 035 $a(PPN)189492805 035 $a(EXLCZ)993450000000004138 100 $a20160829d1991 uy 101 0 $aeng 135 $aur||||||||||| 181 $ctxt 182 $cc 183 $acr 200 10$aPhysical and Hydrologic Flow Properties of Fractures Las Vegas, Nevada~%#~151;zion Canyon, Utah~%#~151;grand Canyon, Arizona~%#~151;yucca Mountain, Nevada, Field Trip T385 210 31$a[Place of publication not identified]$cAmerican Geophysical Union$d1991 215 $a1 online resource (ix, 36 pages) $cillustrations 225 1 $aField trip guidebook (International Geological Congress (28th : 1989 : Washington, D.C.)) ;$vT385 300 $aBibliographic Level Mode of Issuance: Monograph 311 $a0-87590-650-8 320 $aIncludes bibliographical references. 330 $aPublished by the American Geophysical Union as part of the Field Trip Guidebooks Series, Volume 385.Fractures are one of the most abundant structures in geology and are found in almost all rocks and soils at or near the Earth's surface. They are found over a wide range of length scales, from micro-fractures within mineral grams (micro-meters) to oceanic-intraplate fractures as much as 5000 km in length. The important role of fractures in fluid transport in the crust has long been recognized by geologists who have studied dikes (fracture conduits for flow of igneous rocks) and mineral veins fracture conduits for precipitation from aqueous Fluids. In studying these paleo-flow systems, little attention has been given to quantification of the flow properties of the system. Until two decades ago, hydrologists (Long, 1983) and petroleum-reservoir engineers (Nelson, 1985) studying fluid flow in rock had recognized the role of fractures only qualitatively. Quantitatively, the mathematics of fracture flow had been considered intractable while the mathematics of porous-media flow through the rock matrix had been developed and refined for almost one hundred ears. Direct observation of the flow properties of rock at field scales demonstrated the inadequacy of the porous media models beyond the scale of laboratory samples. The hydraulic conductivity of fractured bulk rock has been measured to be as much as 8 orders of magnitude greater than matrix hydraulic conductivity measured in laboratory samples of the same intact rock. Clearly, fractures are primary conduits for fluid flow in rock at time scales of economic and practical interest. Quantitative understanding of the physics of flow in individual fractures and fracture networks has become an important research topic with direct applications to contemporary and paleo flow systems. 410 0$aField trip guidebook (International Geological Congress (28th : 1989 : Washington, D.C.)) ;$vT385. 606 $aGroundwater flow 606 $aGroundwater flow$zArizona 606 $aGroundwater flow$zNevada 606 $aGroundwater flow$zUtah 606 $aFaults (Geology) 606 $aJoints (Geology) 615 0$aGroundwater flow. 615 0$aGroundwater flow 615 0$aGroundwater flow 615 0$aGroundwater flow 615 0$aFaults (Geology) 615 0$aJoints (Geology) 676 $a551.49 700 $aBarton$0880609 702 $aHsieh$b P. A. 801 0$bPQKB 906 $aBOOK 912 $a9910830467103321 996 $aPhysical and Hydrologic Flow Properties of Fractures Las Vegas, Nevada~%#~151;zion Canyon, Utah~%#~151;grand Canyon, Arizona~%#~151;yucca Mountain, Nevada, Field Trip T385$91966682 997 $aUNINA