[Sutri. Chiesa della Madonna del Parto]

Référence bibliographique : Weigert, 692

[Tivoli. Tempio di Vesta ; Tempio della Sibilla]

Référence bibliographique : Weigert, 698

[Viterbe. Fontana della Rocca]

Référence bibliographique : Weigert, 746

[Viterbe. Chiesa di Santa Maria della Verità]

Référence bibliographique : Weigert, 742

[Viterbe. Chiesa Santa Maria della Quercia]

Référence bibliographique : Weigert, 741

[Viterbe. Chiesa Santa Maria della Quercia]

Référence bibliographique : Weigert, 739

[Viterbe. Chiesa Santa Maria della Quercia]

Référence bibliographique : Weigert, 740

[Tivoli. Tempio della Sibilla]

Référence bibliographique : Weigert, 697

[Cava de' Tirreni. Abbazia della Trinità della Cava]

Référence bibliographique : Weigert, 73

[Sienne. Palazzo dei Diavoli ; Monumento della Lupa]

Référence bibliographique : Weigert, 671

[Syracuse. Teatro greco]

Référence bibliographique : Weigert, 693

Una visió de la Guerra de Successió des de l'exili: el 'Teatro de desdichas' (Milà, 1716)

El 1716 es publicà a Milà un text que fa una àmplia justificació històrica i política de la causa de Carles III d'Àustria a la Guerra de Successió d'Espanya (1702-1715). L'obra, de dimensions considerables (72 pàgines), va ser redactada per un eclesiàstic castellà que participà a la defensa de Barcelona durant el darrer setge i que va ser desterrat a Itàlia per les noves autoritats borbòniques. L'article analitza algunes de les idees centrals del text, com ara: l'oposició a la tirania borbònica i la defensa d'una monarquia moderada; la identificació de l'entronització de Felip V com el trencament de l'equilibri europeu i el punt culminant de la decadència d'Espanya; la denúncia de la traïció dels aliats; la vindicació de l'austriacisme castellà i la crítica al borbonisme d'alguns sectors catalans; i la descripció de la repressió i de l'exili.

LUGARESI, Leonardo, Il teatro di Dio. Il problema degli spettacoli nel cristianesimo antico (II-IV secolo), ed. Morcelliana, Brescia, 2008, 895 p., ISBN: 978-88-372-2257-4

La relación del cristianismo con los espectáculos de la tradición romano-pagana, y muy especialmente las críticas que los Padres de la Iglesia dirigieron a todo tipo de manifestación lúdica, constituye un tema complejo y lleno de interés que desde hace unos cuarenta años ha generado la publicación de importantes monografías consagradas a este sujeto. Sin duda, un momento de inflexión fue la aparición, en 1972, del célebre libro de Werner Weismann, Kirche und Schauspiele. Die Schauspiele im Urteil der lateinischen Kirchenväter unter besonderer Berücksichtigung vom Augustin. Posteriormente han visto la luz nuevos trabajos dedicados a examinar esta cuestión.

Juxtaposition of melt impregnation and high-temperature shear zones in the upper mantle; field and petrological constraints from the Lanzo peridotite (Northern Italy)

Results of a field and microstructural study between the northern and the central bodies of the Lanzo plagioclase peridotite massif (NW Italy) indicate that the spatial distribution of deformation is asymmetric across kilometre-scale mantle shear zones. The southwestern part of the shear zone (footwall) shows a gradually increasing degree of deformation from porphyroclastic peridotites to mylonite, whereas the northeastern part (hanging wall) quickly grades into weakly deformed peridotites. Discordant gabbroic and basaltic dykes are asymmetrically distributed and far more abundant in the footwall of the shear zone. The porphyroclastic peridotite displays porphyroclastic zones and domains of igneous crystallization whereas mylonites are characterized by elongated porphyroclasts, embedded between fine-grained, polycrystalline bands of olivine, plagioclase, clinopyroxene, orthopyroxene, spinel, rare titanian pargasite, and domains of recrystallized olivine. Two types of melt impregnation textures have been found: (1) clinopyroxene porphyroclasts incongruently reacted with migrating melt to form orthopyroxene plagioclase; (2) olivine porphyroclasts are partially replaced by interstitial orthopyroxene. The meltrock reaction textures tend to disappear in the mylonites, indicating that deformation in the mylonite continued under subsolidus conditions. The pyroxene chemistry is correlated with grain size. High-Al pyroxene cores indicate high temperatures (11001030C), whereas low-Al neoblasts display lower final equilibration temperatures (860C). The spinel Cr-number [molar Cr/(Cr Al)] and TiO2 concentrations show extreme variability covering almost the entire range known from abyssal peridotites. The spinel compositions of porphyroclastic peridotites from the central body are more variable than spinel from mylonite, mylonite with ultra-mylonite bands, and porphyroclastic rocks of the northern body. The spinel compositions probably indicate disequilibrium and would favour rapid cooling, and a faster exhumation of the central peridotite body, relative to the northern one. Our results indicate that melt migration and high-temperature deformation are juxtaposed both in time and space. Meltrock reaction may have caused grain-size reduction, which in turn led to localization of deformation. It is likely that melt-lubricated, actively deforming peridotites acted as melt focusing zones, with permeabilities higher than the surrounding, less deformed peridotites. Later, under subsolidus conditions, pinning in polycrystalline bands in the mylonites inhibited substantial grain growth and led to permanent weak zones in the upper mantle peridotite, with a permeability that is lower than in the weakly deformed peridotites. Such an inversion in permeability might explain why actively deforming, fine-grained peridotite mylonite acted as a permeability barrier and why ascending mafic melts might terminate and crystallize as gabbros along actively deforming shear zones. Melt-lubricated mantle shear zones provide a mechanism for explaining the discontinuous distribution of gabbros in oceancontinent transition zones, oceanic core complexes and ultraslow-spreading ridges.