01094nam--2200373---450 99000161927020331620201209090334.088-15-07083-4000161927USA01000161927(ALEPH)000161927USA0100016192720040429d1999----km-y0itay0103----baitaIT||||||||001yyIstruire nelle verità repubblicanela lettura politica per il popolo nell'Italia in rivoluzione1769-1799Luciano GuerciBolognaIl Mulino1999374 p.22 cmSaggi4962001Saggi4962001001-------2001Letteratura1769-1799850.6GUERCI,Luciano139844ITsalbcISBD990001619270203316X.2.B. 646(III D 607)147167 L.M.III DX.2.B. 646a(III D 607bis)21679 L.M.III DBKUMAIstruire nelle verità repubblicane222482UNISA05373nam 22006734a 450 991102043130332120200520144314.01-280-28546-X97866102854641-4443-0445-31-4051-2910-7(CKB)1000000000342128(EBL)428306(SSID)ssj0000241140(PQKBManifestationID)11235633(PQKBTitleCode)TC0000241140(PQKBWorkID)10267193(PQKB)11105701(MiAaPQ)EBC428306(MiAaPQ)EBC4956650(Au-PeEL)EBL4956650(CaONFJC)MIL28546(OCoLC)711274148(EXLCZ)99100000000034212820021025d2003 uy 0engur|n|---|||||txtccrSandstone diagenesis recent and ancient /edited by Stuart D. Burley and Richard H. WordenMalden, MA Blackwell Pub.20031 online resource (664 p.)Reprint series volume 4 of the International Association of SedimentologistsDescription based upon print version of record.1-4051-0897-5 Includes bibliographical references and index.SANDSTONE DIAGENESIS: Recent and Ancient; Contents; Introduction; Sandstone diagenesis: the evolution of sand to stone; Eogenesis (early diagenesis); Marine eogenesis; Formation of siderite-Mg-calcite-iron sulphide cconcretions in intertidal marsh and sandflat sediments, north Norfolk, Englan; Origin of authigentic carbonates in sediment from the deep Bering Sea; De glauconiarum origine; Low-Mg calcite marine cement inCretaceous turbidites: origin, spatial dis-tributionand relationship to seawaterchemistry; The concretions of the BearreraigSandstone Formation: geometry and geo-chemistryNon-marine eogenesis 1: warm and wet environmentsThe anatomy of an early Dinantian ter-racedfloodplain: palaeo-environmentand early diagenesis; Early diagenetic, siderite as an indicator of depositional environment in the Triassic Rewan Group, southern Bowen Basin, eas; Early diagenetic spherulitic siderites from Pennsylvanian palaeosols in the Boss Point Formation, Maritime Canada; Early diagenesis and its relationship to depositional environment and relative sea-level fluctuations; Non-marine eogenesis 2: arid environments; Diagenetic alunite in clastic sequences, Kuwait, Arabian GulfNodular silcretes of the Cypress Hills Formation (upper Eocene to middle Miocene) of southern Saskatchewan, CanadaRock varnish in the Sonoran Desert: microbiologically mediated accumulation of manganiferous sediments; Models of rock varnish formation constrained by high resolution transmission electronic microscopy; Calcretes related to phreatophytic vegetation from the Middle Triassic Otter Sandstone of South West England; Zeolitic diagenesis of late Quaternary fluviolacustrine sediments and associated calcrete formation in the Lake Bogoria Basn,Groundwater dolocretes from the Upper Triassic of the Paris Basin, France: a case study of an arid, continental diagenetic faMesogenesis (burial diagenesis); Quartz-related mesogenesis; Formation of quartz overgrowths in the Penrith sandstone (Lower Permian) of northwest England as revealed by scanning electro; A scale of dissolution for quartz and its implications for diagenetic processes in sandstones; Thin section and S.E.M. textural criteria for the recognition of cement-dissolution porosity in sandstonesA numerical model for porosity modification at a sandstone-mudstone boundary by quartz pressure dissolution and diffusive masOrigin of quartz cements in some sandstones from the Jurassic of the Inner Moray Firth (UK); Carbonate-cement-dominated mesogenesis; Geochemistry of carbonate cements in the Sag River and Shublik Formations (Triassic/Jurassic), North Slope, Alaska: implicati; Burial dolomitization and porosity development in a mixed carbonate-clastic sequence: an example from the Bowland Basin, nort; Clay and aluminosilicate mineral-related mesogenesisDIAGENETIC ORIGIN OF GRAYWACKE MATRIX MINERALSDiagenesis affects all sediments after their deposition and includes a fundamental suite of physical, chemical and biological processes that control the texture, mineralogy and fluid-flow properties of sedimentary rocks. Understanding the processes and products of diagenesis is thus a critical component in the analysis of the evolution of sedimentary basins, and has practical implications for subsurface porosity destruction, preservation and generation. This in turn is of great relevance to the petroleum and water industries, as well as to the location and nature of some economic mineral deposReprint series ... of the International Association of Sedimentologists ;v. 4.SandstoneDiagenesisSandstone.Diagenesis.552/.5Burley Stuart D930047Worden Richard H878737MiAaPQMiAaPQMiAaPQBOOK9911020431303321Sandstone diagenesis2252743UNINA02621nam 2200433z- 450 991029580680332120260329165614.02-490296-20-5(CKB)4100000007205253(oapen)https://directory.doabooks.org/handle/20.500.12854/59048(oapen)doab59048(EXLCZ)99410000000720525320202102d2011 |y 0freurmn|---annantxtrdacontentcrdamediacrrdacarrierSe vêtir À LA COUR EN EUROPE 1400-1815Cultures matérielles, cultures visuelles du costume dans les cours européennesPublications de l'Institut de recherches historiques du Septentrion20111 online resource2-905637-64-1 C'est à la cour, lieu du paraître par excellence, que s'exprime le plus la préoccupation des sociétés pour les apparences. Que signifie la façon de se vêtir dans cette « société du spectacle » ? Le paraître vestimentaire y est un puissant moteur de pratiques culturelles qui touchent au corps et à l'identité. Il active toute une économie du luxe et alimente la dynamique des échanges entre les cours européennes. Cet ouvrage aborde le vestiaire des princes et de leurs courtisans entre 1400 et 1815, en plein essor de la société curiale. Les souverains ont été parmi les premiers à avoir pris conscience du pouvoir de l'habit et l'ont porté au plus haut degré de raffinement. Se vêtir, c'est aussi régner et gouverner. Loin d'être figé par un système contraignant de codification des apparences, l'habit de cour se définit en fonction de la mode dans laquelle il joue un rôle décisif, notamment en matière de circulations internationales. Élément d'une culture matérielle somptueuse du passé, l'habit de cour perdure dans notre culture visuelle. Sur les podiums de la haute couture ou à l'écran, il reformule des apparences qui relevaient, en leur temps, elles aussi, de la performance des corps et des textiles.Se vêtir À LA COUR EN EUROPE 1400-1815 Biography and non-fiction prosebicsscapparencecostumecourcourtisansmœursroisouverainBiography and non-fiction proseIsabelle Paresysauth1228413Natacha CoqueryauthBOOK9910295806803321Se vêtir À LA COUR EN EUROPE 1400-18153041233UNINA01131nlm 2200313Ia 450 99664897010331620250325101444.019840601d1694---- uy |engUKdrcnu<<A>> postscript to a book published last year entituled Considerations on Dr. Burnet's Theory of the earthLondonPrinted and are to be sold by Randal Taylor1694Testo elettronico (PDF) (8 p.)Base dati testualeTitolo della didascaliaPagina 7 firmata: John Beaumont, JunRiproduzione dell'originale nella British LibraryAltri collaboratori: Burnet, Thomas, 1635?-1715.; Beaumont, John, m. 1731.CreazioneBNCF202.4BEAUMONT,Johnd. 1731.1008580BURNET,Thomas1635?-1715.795616ITcbaREICAT996648970103316EBERPostscript to a book published last year entituled Considerations on Dr. Burnet's Theory of the earth4343081UNISA