1,721,169 research outputs found
aida annali italiani del diritto d'autore, della cultura e dello spettacolo . Anno XXIX (2020)
No full textAnna Fubelli ha trascritto diversi documenti sui contratti tra Giuseppe Verdi e l'editore Ricordi relativi a 9 opere del famoso musicista italiano. Nella sua prefazione Anna Fubelli elenca i criteri da lei utilizzati per la selezione e la trascrizione dei documenti. Luigi Carlo Ubertazzi ha aggiunto una breve prefazione sull'importanza della trascrizione e pubblicazione di questi documenti contrattuali: tra l'altro, per l'importanza dell'autore Giuseppe Verdi e la mancanza di pubblicazioni di documenti italiani sulla storia dei contratti relativi ad opere protette da copyright nel Ottocento, oltre che per alcune interessanti indicazioni che i documenti qui pubblicati offrono sulla storia dei contratti sul diritto d'autore italiano.Anna Fubelli transcribed several documents on contracts between Giuseppe Verdi and the publisher Ricordi relating to 9 operas by the famous Italian musician. In her preface Anna Fubelli listed the criteria she used for selecting and transcribing the documents. Luigi Carlo Ubertazzi added a short preface on the importance of the transcription and publication of these contractual documents: inter alia, for the importance of the author Giuseppe Verdi and the lack of publications of Italian documents on the history of contracts relating to copyrighted works in the nineteenth century, as well as for some interesting indications that the documents herein published offer about the history of contracts on Italian copyright
Musica come prodotto dell'ingegno e tutela del diritto d'autore nel sistema operistico italiano dell'Ottocento
Full text linkAnna Fubelli ha trascritto diversi documenti sui contratti tra Giuseppe Verdi e l'editore Ricordi relativi a 9 opere del famoso musicista italiano. Nella sua prefazione Anna Fubelli ha elencato i criteri utilizzati per la selezione e la trascrizione dei documenti ed esposto l'importanza della trascrizione e pubblicazione di questi documenti contrattuali: tra l'altro, per l'importanza dell'autore Giuseppe Verdi e la mancanza di pubblicazioni di documenti italiani sulla storia dei contratti relativi ad opere protette da diritto d'autore nell'Ottocento, nonché per alcune interessanti indicazioni che i documenti qui pubblicati offrono sulla storia dei contratti sul diritto d'autore italiano
Comment on: “Geomorphological, paleontological and 87Sr/86Sr isotope analyses of early Pleistocene paleoshorelines to define the uplift of Central Apennines (Italy)”
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Drainage system adjustment in response to the opening of the Rieti intermontane basin (Central Italy): geostatistical reconstruction of the PaleoFarfa River alluvial plain
No full textThe Rieti intermontane basin is one of the western tectonic depressions of the Central Apennines. Its infilling deposits are currently cut by the Farfa River, a left tributary of the Tiber River with a 132 km2 wide drainage basin. It currently flows from the Sabini Mts. (Central Apennines) into the Tiber River to the WSW. In the upper basin, the river cuts fluvial conglomerates and sands, which are Gelasian in age. Downstream, on the left side of the Tiber Valley, the facies show deltaic to clearly marine characteristics that indicate the presence of the Gelasian paleo-shoreline, which is also indicated by the finding of Lithodomus holes in the calcareous bedrock at an elevation of 260-277 m a.s.l. The shape of the Gelasian alluvial plain and delta has been outlined and redrawn via GIS techniques. We herein underline that during the Gelasian, the shoreline was located at the foot of the Fara in Sabina Mts. and that the alluvial plain of the PaleoFarfa River was much wider (approximately 700 km2) than the present, extending to the foot of the Reatini Mts. The reconstruction of both the basal and top surfaces of the old alluvial body provides evidence that the activity of Quaternary faults, responsible for the formation of the Rieti intermontane basin, strongly influenced the deposition of the alluvial body and finally caused the adjustment of the PaleoFarfa drainage system. Finally, from the shoreline elevation, a Pleistocene averaged uplift rate of 0.12/0.14 mm/year has been calculated for this sector of the Apennines. © 2014 Accademia Nazionale dei Lincei
Morphometric evidence of the topographic growth of central Apennines
No full textOn the basis of DEM analysis, we examine the tectonic geomorphology
of the Apennines in central Italy to figure out the topographic
evidence for how Apennines landscape was shaped by its emergence
above sea level, in the tectonic context of a growing mountain chain.
Geologic and geomorphic data suggest that its topographic growth was
slow during the phase of crustal shortening (Miocene-Pliocene), but accelerated
at the end of lower Pleistocene, when tectonics was already
dominated by extension. Such different uplift rates should influence the
development of the resulting landforms. We investigate the topography
and the drainage features of a E-W transect across central Italy, focusing
on topographic metrics, drainage pattern and stream long profiles.
The results indicate that the Apennines topography is characterized by
the superimposition of a short wavelength (10-30 km wide spacing),
linked to local tectonic structures (extensional on the Tyrrhenian side
and compressive on the Adriatic side), and a long one that corresponds
to a broad topographic bulge 200-300 km wide, that records a regional
uplift. As a response, the rivers incised the topography of the growing
chain mostly the same and, interacting with climate changes, generated
at least three major inset alluvial terraces. In particular, on the Tyrrhenian
side, the rectangular drainage pattern indicates the strong influence
of the extensional tectonics. This is also evident in the stream long profiles,
where knickpoints and knickzones correspond with tectonic lineaments
and extensional basins respectively. The hydrographic network
draining to the Adriatic Sea shows a parallel pattern. The knickpoints
of the stream long profiles generally correspond to rock changes and to
very deep and narrow gorges, where the rivers incised the compressive
structures reaching their cores. A high-resolution DEM of an area just
south of Ancona provided information at a nested scale of observation.
This region contains two major low relief surfaces. The one at higher elevations
is located at the crest of the chain cutting across carbonates
and marls. The other surface is inset into the flanks of the range and
mostly cuts across turbidites. A third geomorphic surface, located more
eastward, is underlain by Pliocene and Quaternary deposits. Coupling
the morphometry analysis, the map of Pliocene-lower Pleistocene deposits,
and previous studies, we explore the relationships among the landscape features, the regional vertical tectonism, and the local deformational
processes. The results are consistent with a landscape dominated
by the broad Quaternary uplift superimposed on local tectonics,
suggesting new constrains for the long term evolution of the landscape
of central Italy in the context of the Apennines topographic growth
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