1,370,651 research outputs found
Albert Russell Ascoli, Dante and the Making of a Modern Author, Cambridge UK, University Press, 2008
No full textZetemata Alexandrou tou Aphrodisieos physika, peri psyches, ethika : Metaphrasis ek ton Damasiou eis to proton Peri ouranou biblion ; Epitome scholike eis ta d' prota kai to é Peri physikes biblia ; Theophrastou Peri aistheseos biblion ; Priskuaiou lydou metaphrasis ton Theophrastou Peri aistheseos kai phantasias = Quaestiones Alexandri Aphrodisiensis naturales, de anima, morales : Metaphrasis ex Damascio in primum librum De coelo & mundo ; Epitome per modum comentarij in quatuor primos, & octauum physices libros ; Theophrasti liber De sensu ; Prisciani lydi metaphrasis in libros Theophrasti De sensu & phantasia
Full text linkA diferencia de lo indicado en la portada, la edición contiene, además de las Quaestiones (h. [II]v-XXXVIIIv), el tratado de Alejandro de Afrodisias, De fato (h. XXXIXr-XXXXVIIIr)El ed. lit. es Vittore Trincavelli, cuyo nombre consta en prefacioLugar e imp. deducidos de la marcaSign.: a-f8. -- L. red. en prefacio. -- Tipos griegos. -- ReclamosMarca tip. xil. en port. de Bartolomeo Zanetti. -- En a3r friso e inic. en rojoTexto en griego y prefacio en latínXXXXVIII h. ; Fol
Il nuovo quadro istituzionale e legislativo
No full textIl saggio si articola in cinque paragrafi, dei quali il secondo e il quinto redatti da L. Zanetti, il terzo e il quarto redatti da G. Piperata, mentre il primo paragrafo è comune
'Serie del Encuentro', primera colección del CEAL: Entrevista a Susana Zanetti
No full textFil: Zanetti, Susana. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.Fil: Cilento, Laura. Universidad Nacional de Quilmes; Universidad Nacional de San Martín
Xylodromus segmentarius Zanetti 2014, n. comb.
No full text<i>Xylodromus segmentarius</i> (Mäklin, 1852) n. comb. <p> <i>Omalium segmentarium</i>: Mäklin, 1852: 322.</p> <p> <i>Anthobium segmentarium</i> (Mäklin); Fauvel 1878: 200; Bernhauer and Schubert 1910: 43. <i>Eusphalerum segmentarium</i> (Mäklin); Moore and Legner 1975: 191; Herman 2001: 454.</p> <p> <b>Examined type material.</b> Holotype male Sitcha/Holmberg/166 [?]/ Omalium segmentarium Mäkl. /Mus. Zool. H:fors/Spec. typ. 2127/Mus. Hels. N:o 1766/ Xylodromus segmentarius (Mäklin 1852) det. A. Zanetti 2013/ Holotypus (red) (MZH).</p> <p> This species described from “insula Sitkha” (Alaska) was included in <i>Eusphalerum</i> (as <i>Anthobium</i>) by Fauvel on the basis of the form of the elytral apex (“... ad angulum interiorem apice producta; verisimile ad differentiam sexualem spectat;” (Mäklin, 1852). The examination of the type demonstrates that the species belongs to the genus <i>Xylodromus</i> Heer, 1839 (Fig. 153) and that it is not a junior synonym either of <i>Xylodromus concinnus</i> (Marsham, 1802) or of <i>Xylodromus depressus</i> (Gravenhorst, 1802), European species both also reported from North America. The validity of <i>Xylodromus capito</i> (Casey, 1894) (type from Wisconsin) requires examination of the type.</p>Published as part of <i>Zanetti, Adriano, 2014, Taxonomic revision of North American Eusphalerum Kraatz, 1857 (Coleoptera, Staphylinidae, Omaliinae), pp. 1-80 in Insecta Mundi 2014 (379)</i> on page 59, DOI: <a href="http://zenodo.org/record/5179446">10.5281/zenodo.5179446</a>
Vettore Zanetti Zilla: A Murano
No full textScheda tecnica e storico artistica dell'opera di Vettore Zanetti Zill
Conversazioni moscovite
No full textArchitettura di Mosca nel XX secolo. Evoluzioni, influenze, riscontri sociali e culturali
Zanetti critico d’arte: dalla Descrizione di tutte le pubbliche pitture a Della pittura veneziana
No full textIl contributo analizza le posizioni critiche di Anton Maria Zanetti alla luce del confronto tra le sue due principali opere storiografiche. Obiettivo generale è comprendere come lo storiografo giunga a scrivere il Della pittura veneziana e quali siano le caratteristiche intrinseche del testo contenuto in un libro pensato esplicitamente per orientare il pubblico alla
conoscenza della pittura della città. Attenzione specifica è dedicata ai Proemi e alle Premesse, in cui l’autore esplicita i propri intenti metodologici; un'attenta analisi del lessico utilizzato, contente inoltre di cogliere le novità di metodo e di posizioni critiche di Zanetti, così come erano percepite dai contemporanei. Le posizioni critiche espresse nei testi a stampa sono infine messe a confronto con le Note de’ quadri manoscritte, che raccolgo l'attività di Zanetti come Ispettore alle Pubbliche Pitture della città di Venezia
Origin and significance of late noritic dykes in the Baldissero Peridotite Massif (Ivrea-Verbano zone)
No full textThe Baldissero Peridotite Massif (Southern Ivrea-Verbano Zone) is a depleted lherzolite (ol 65/70, opx 16/20, cpx 10/11, sp 2/2.5, La(N)/Yb(N) 0.003/0.26, ε(Nd)270 = 6.4/14, 87Sr/86Sr = 0.7021/0.7035). It is cross-cutted by a swarm of 5/15 cm thick, fine grained (<1mm), NNE trending noritic dykes. Contacts peridotite-dyke are sharp. Dyke texture is hypidiomorphic and their mode consists of dominant plagioclase (31/45 %, An 40/48), orthopyroxene (25/37%, En = 78.9/87.8, Wo = 0.6/1.1), subordinate clinopyroxene (14/18%, En = 42.7/44.0, Wo = 47.9/52.4), interstitial pargasitic amphibole (10/15%) and opaques (1/2%, Fe-Ni sulfides). Re-equilibration conditions are 0.8/1 GPa and 800/900°C, like those of the ambient peridotite. Major element (wt%) dyke composition is characterized by high MgO (10/16) and high Mg values (0.81/0.89). In the observed MgO range, SiO2, CaO and K2O vary negligibly (52/53, 9/10 and <0.2, respectively). With decreasing MgO, TiO2 varies randomly from 0.8 to 0.4, Al2O3 increases from 15 to 21, Na2O from 3 to 4.5 and FeO decreases from 5 to 2. Bulk rock incompatible trace element patterns (Fig. 1) vary from weakly LREE depleted to weakly LREE enriched (La(N)/Yb(N) = 0.5/2.4) and have marked positive Sr anomaly (Sr/Sr(*) = 5.6/10.4), smaller Eu anomaly (Eu/Eu(*) 1.3/1.5) and negative Nb anomaly (La(N)/Nb(N) = 1.2/2.2). Incompatible element concentration increases, and the magnitude of the negative Nb and of the positive Sr anomalies decrease, with increasing MgO or Mg. Main incompatible trace element carriers are clinopyroxene and hornblende, which display patterns varying from slightly LREE depleted to enriched. Orthopyroxene is LREE depleted and plagioclase is LREE and Sr enriched. Clinopyroxene is Nb-depleted (La(N)/Nb(N) = 1.0/5.9) and amphibole is Nb enriched (La(N)/Nb(N) = 0.09/0.35). The latter phases have negative Zr spikes. Incompatible element concentration in the mafic phases show correlations with Mg similar to those of bulk rock (Fig. 2). The only available isotope determination refers to a Sm-Nd internal isochron which results in an age of 180Ma and ε(Nd) = 7.8. In spite of the contacts being sharp, peridotite mineral assemblage and composition varies over a distance of 7 cm. In the peridotite, toward the dyke contact, modal orthopyroxene increases and clinopyroxene decreases, whereas trace element concentration and La(N)/Yb(N) increase (from 0.003/0.017 to 0.1/0.26) and Mg decreases from 0.9 to 0.8. The dyke at the peridotite contact does not show sizeable chemical or modal variations. There is no clear relationship between the Mg variation of the dyke and the chemical trends observed in the contact peridotite. The high Mg numbers of the dykes and the Mg value of orthopyroxene, lower than that of bulk-rock, indicate that these norites are not melts, but rather represent mineral segregates possibly retaining some interstitial liquid. Estimates of the Mg values of the parental melts, made assuming (opx/liq)D(Mg) = 1.2, indicates a Mg range from 0.66 to 0.74, which is consistent with that of primary mantle-derived magmas. Since olivine does not occur even in the more MgO-rich dyke composition, the parent melt had to be, furthermore, SiO2-rich and hydrous, as indicated by the amphibole abundance. Whatever the set of solid/melt partition coefficient used for estimating trace elements in the parent melts, the calculated REE profiles would vary from slightly LREE depleted to variably LREE enriched. The HFSE characteristics of the primary melts cannot be precisely constrained because of the strong dependence of their partition coefficient on the melt composition. For example, using available partition coefficients for basaltic compositions, the estimated parental melts would have a weak Nb and Zr anomaly, which disappears using D sets for intermediate compositions and become positive if the D's are referred to high-silica compositions. In any case, the geochemical trends shown by bulk rock and mineral phases (i.e. the increase of incompatible element concentration with increasing Mg) are qualitatively maintained. We propose that this peculiar feature can be explained either by fluid-assisted melting of a depleted peridotite source, where melting degree increases with the increasing supply of hydrous fluid (which is the incompatible element carrier), or by fluid-peridotite reaction during porous flow percolation in a mantle column at a deeper and higher temperature level than that actually observed. If confirmed by new isotopic data, the occurrence of post-Hercynian gabbroic rocks in the Australpine and South Alpine domains will support the involvement of the marginal units of the Adria plate in the pre-oceanic extensional regime (Piccardo et al., 1994)
- …
