00896nam2-22003011i-450-99000373920040332119991111000000.018-615-2015-8000373920FED01000373920(Aleph)000373920FED0100037392020010215d1999----km-0yitaA0103----baENGGB<<The >>dynamics of international strategySusan Segal-Horn and David FaulknerLondon [etc.]International Thomson business press[1999]X, 286 p.24 cmGBLondon [etc.]Segal-Horn,Susan141742Faulkner,David<1938- >117597ITUNINARICAUNIMARCBK9900037392004033214-9-675-TI7124ECAECADynamics of international strategy509128UNINA02282nam0 2200373 450000003715120250211194018.0978-88-351-4630-8e-book pdf20250211d2023----km-y0itay50------baitaITy-------001yysdoug----uuuuu<<La >>contabilizzazione dell'avviamento tra impairment e ammortamentorisorsa elettronicariflessioni ed evidenze empiricheFrancesco Avallone, Lorenzo SimoniMilanoAngeli2023184 p.23 cm1 testo elettronicoTheory and practice in accounting, auditing and risk management4Dati testuali (1 file)Modalità di accesso: World Wide WebIndice del libro free access:http://digital.casalini.it/9788835152996Il volume vuole fornire un contributo al dibattito sul trattamento contabile dell'avviamento, presentando una riflessione sulla definizione di tale elemento e sulla capacità del bilancio di catturarlo adeguatamente. In particolare, il libro illustra i pregi e i limiti dell'attuale trattamento incentrato sul solo impairment, le proposte di riforma e i principali risultati empirici forniti dalla letteratura. Sulla base di tali evidenze, il testo propone una simulazione degli effetti di un ipotetico ammortamento dell'avviamento. [Testo dell'editore]2001Theory and practice in accounting, auditing and risk management4<<La >>contabilizzazione dell'avviamento tra impairment e ammortamento4312097ImpreseAvviamento d'azienda <Diritto italiano>Avviamento commercialeContabilità657.723Contabilità per specifiche fasi di attività aziendaleAvallone,Francesco<1975- >0701373915Simoni,Lorenzo0701783767ITUNIPARTHENOPE20250211RICAUNIMARChttp://digital.casalini.it/9788835152996Accesso limitato alla rete di Ateneo Università di Napoli "Parthenope"Data ultima consultazione: 2025-02-11000037151E-BOOK49891NAVA12025Contabilizzazione dell'avviamento tra impairment e ammortamento4312097UNIPARTHENOPE03726nam 22005055 450 991033788950332120200630115304.03-030-00166-010.1007/978-3-030-00166-7(CKB)4100000006674803(MiAaPQ)EBC5526653(DE-He213)978-3-030-00166-7(PPN)230540511(EXLCZ)99410000000667480320180925d2019 u| 0engurcnu||||||||txtrdacontentcrdamediacrrdacarrierGeological Records of the Fuegian Andes Deformed Complex Framed in a Patagonian Orogenic Belt Regional Context /by Rogelio Daniel Acevedo1st ed. 2019.Cham :Springer International Publishing :Imprint: Springer,2019.1 online resource (116 pages) illustrationsSpringerBriefs in Earth System Sciences,2191-589X3-030-00165-2 Includes bibliographical references.1:Introduction -- 2:Background -- 3:The geological formations of the Mesozoic complex -- 4:The basic eruptive rocks of the Alvear and Sorondo ranges (Mount Olivia) -- 5:The Cretaceous layers younger than the Early Cretaceous -- 6:The estimated basement for the Fuegian Andes Mesozoic stratigraphic series and the rocks considered to be as of pre-Mesozoic age -- 7:A synthesis about the stratigraphic, formational problem -- 8:A simplified view about the Fuegian Andes and the complex folding of the Mesozoic and Early Tertiary units -- References.The Fuegian Andes in Argentina show both simple and complex aspects. The first ones refer to the general stratigraphy of the area and the latter result from their tectonic characteristics. Concerning the stratigraphy, an appraisal of the denomination and valorization of formations of Jurassic and early Cretaceous age is performed here to reach the simple scheme of the Fuegian-Patagonian continuity under the name of “Fuegian Andes Deformed Complex”. As an essay the formational nomenclature is simplified and the local concept of basement is evaluated. In relation to their structural aspects it is assumed that the formation of the orogenic Fuegian arc and the folding of the Mesozoic and early Tertiary layers are connected phenomena. Tectonic forces from the West, the Northeast and the South have had participation in the formation of the tectonic arc. The lithostatic column pressure was added once the layers were folded and thrusted upwards during the birth of the Fuegian Andes. Even the speculation of a great main fold overturned to North, as an abstraction, is considered. Instead, the Magallanes-Fagnano fault is appreciated only as a product of the transcurrent Quaternary movements, lacking associated eruptive processes that contribute to define plate borders.SpringerBriefs in Earth System Sciences,2191-589XGeology, StructuralSedimentologyStructural Geologyhttps://scigraph.springernature.com/ontologies/product-market-codes/G17040Sedimentologyhttps://scigraph.springernature.com/ontologies/product-market-codes/G17080Geology, Structural.Sedimentology.Structural Geology.Sedimentology.551.8558.276Acevedo Rogelio Danielauthttp://id.loc.gov/vocabulary/relators/aut979422BOOK9910337889503321Geological Records of the Fuegian Andes Deformed Complex Framed in a Patagonian Orogenic Belt Regional Context2232940UNINA