In principio erat liber : l'organisation du premier livre de motets de Tomás Luis de Victoria (Venise, 1572)

L'organisation du premier livre de motets de Tomás Luis de Victoria, publié à Venise en 1572 chez les Fils d'Antonio Gardano (RISM V 1421), repose sur une stratification d'éléments divers mais complémentaires. Les pièces sont organisées en quatre groupes : quatorze à 4 voix, neuf à 5 voix, neuf à 6 voix et une à 8 voix. Elles forment des paires modales. Les derniers motets des groupes reposent sur des écritures individualisées (ad aequales, canon à l'unisson, Tenormotette, motet à double choeur). De plus, un jeu avec le nombre de parties, une et deux essentiellement, intervient entre les groupes et à l'intérieur. Les textes émanent de plusieurs rites (avilais, prétridentin et tridentin) et sources. Lorsque c'est nécessaire, le compositeur les remanie pour qu'ils s'adaptent à l'organisation du recueil. Au bout du compte, le livre veut être un objet ayant un certain poids et qui dit quelque chose de plus qu'une simple addition de pièces. C'est précisément ce dont a besoin le jeune compositeur pour prendre une place sur le marché du motet avec ce qui constitue son premier « opus ». Dans la dédicace qu'il signe lui-même, Victoria inscrit son édition dans la mouvance de la musica reservata puisqu'il la destine d'abord aux connaisseurs. Or, c'est précisément cette organisation complexe qui permet au musicien d'inscrire son recueil dans une lignée de publications savantes, initiées semble-t-il par le livre de motets à 5 voix d'Adrian Willaert, qui date de 1539.

Un Taller de grabado sostenible

Ponència presentada al "Encuentro internacional de grabado no tóxico", 2009, Monterrey, Nuevo León, México

La seguridad en el taller de grabado

Ponència presentada a la Jornada de Recerca en Educació per a la Sostenibilitat, Xarxa EDUSOST, 25 de novembre de 2011, Universitat de Barcelona, Barcelona.

Vicente Cacho Viu (1929-1997), in memoriam

On the occasion of the recent death of the madrilenian culture historian Vicente Cacho Viu, the authors expose the main lines of his historical work. They point out the importance of Cacho's research on the periord of the Restauración, mainly his studies on the liberal education institution Institución Libre de Enseñanza. They also consider Cacho's interest in Catalonia, remembering the time he spent teaching at Barcelona University, paying attention to his works on catalan modernisme. The article includes a systematic bibliography of Cacho's works.

Vicente Cacho Viu (1929-1997), in memoriam

On the occasion of the recent death of the madrilenian culture historian Vicente Cacho Viu, the authors expose the main lines of his historical work. They point out the importance of Cacho's research on the periord of the Restauración, mainly his studies on the liberal education institution Institución Libre de Enseñanza. They also consider Cacho's interest in Catalonia, remembering the time he spent teaching at Barcelona University, paying attention to his works on catalan modernisme. The article includes a systematic bibliography of Cacho's works.

La cartografía del Estado Mayor del Ejército de Tierra republicano durante la Guerra Civil española. El archivo del general Vicente Rojo

En los últimos años, se ha llevado a cabo un considerable esfuerzo de análisis y catalogación de la ingente cantidad de mapas militares, planos, croquis y vistas panorámicas realizados durante la Guerra Civil española, pero aún quedan múltiples aspectos por investigar. En este artículo, analizamos la formación cartográfica del general Vicente Rojo -el jefe del Estado Mayor del Ejército de Tierra republicano-, las relaciones de Rojo con la cartografía durante la Guerra Civil y la cartografía militar contenida en su archivo personal, que se custodia en el Archivo Histórico Nacional de Madrid. Dicha cartografía posee un gran valor cartográfico y militar, porque fue utilizada por el Estado Mayor del Ejército de Tierra republicano durante el período en que Rojo estuvo al frente del mismo, y porque contiene una serie de documentos cartográficos manuscritos inéditos de gran importancia para comprender el desarrollo de algunas de las operaciones bélicas principales.

Who wrote the Second Ave maris stella of Tomás Luis de Victoria?

Contrary to what Felipe Pedrell indicates, the second Ave maris stella in his Victoria's collected works (vol. V, 1908, pp. 100-3, n° 33) doesn't appear in the collection published in 1600 in Madrid by the composer, nor in any other of the musician's books. In the 1600 edition, Victoria reissues the two first verses (plainchant followed by polyphony) of the Ave maris stella published in 1576 and then again in 1581. The earliest source of the problematic Ave maris stella is Munich, Bayerische Staatsbibliothek, Musik-Abteilung, 2 Mus. pr. 23 handschriftlicher Beiband, dating from the third quarter oft he seventeenth century. This source is a manuscrit that runs as an appendix to the 1581 edition of Victoria's hymns. No attributions are given in the manuscript. The first attributions of the piece to Victoria arise in the nineteenth century, in manuscripts copied by Johann Michael Hauber, Johann Caspar Aiblinger, August Baumgartner and Carl Proske, and preserved in Munich and Regensburg. Proske pubished the piece in his Musica divina in 1859 (Annus primus, vol. III, pp. 419-24). The most probable hypothesis ist that Pedrell had knowledge of the second Ave maris stella, under the spanish composer's name, via Proske's Musica divina. In all likelihood the piece is not by Victoria, not least because the composer has never written odd polyphonic verses of hymns. In his Studies in the Music of Tomás Luis de Victoria (2001), Eugene Casjen Cramer relies on the supposed authenticity of the work to ascribe the others pieces of Munich, Bayerische Staatsbibliothek, Musik-Abteilung, 2 Mus. pr. 23 handschriftlicher Beiband to the composer. These attributions should therefore be refuted.

An evaluation of the inorganic and organic geochemistry of the San Vicente Mississippi Valley-type zinc-lead district, central Peru: Implications for ore fluid composition, mixing processes, and sulfate reduction

Mississippi Tialley-type zinc-lead deposits and ore occurrences in the San Vicente belt are hosted in dolostones of the eastern Upper Triassic to Lower Jurassic Pucara basin, central Peru. Combined inorganic and organic geochemical data from 22 sites, including the main San Vicente deposit, minor ore occurrences, and barren localities, provide better understanding of fluid pathways and composition, ore precipitation mechanisms, Eh-pH changes during mineralization, and relationships between organic matter and ore formation. Ore-stage dark replacement dolomite and white sparry dolomite are Fe and rare earth element (REE) depleted, and Mn enriched, compared to the host dolomite. In the main deposit, they display significant negative Ce and probably Eu anomalies. Mixing of an incoming hot, slightly oxidizing, acidic brine (H2CO3 being the dominant dissolved carbon species), probably poor in REE and Fe, with local intraformational, alkaline, reducing waters explains the overall carbon and oxygen isotope variation and the distributions of REE and other trace elements in the different hydrothermal carbonate generations. The incoming ore fluid flowed through major aquifers, probably basal basin detrital units, with limited interaction with the carbonate host rocks. The hydrothermal carbonates show a strong regional chemical homogeneity, indicating access of the ore fluids by interconnected channelways near the ore occurrences. Negative Ce anomalies in the main deposit, that are absent at the district scale, indicate local ore-fluid chemical differences. Oxidation of both migrated and indigenous hydrocarbons by the incoming fluid provided the local reducing conditions necessary for sulfate reduction to H2S, pyrobitumen precipitation, and reduction of Eu3+ to Eu2+. Fe-Mn covariations, combined with the REE contents of the hydrothermal carbonates, are consistent with the mineralizing system shifting from reducing/rock-dominated to oxidizing/fluid-dominated conditions following ore deposition. Sulfate and sulfide sulfur isotopes support sulfide origin from evaporite-derived sulfate by thermochemical organic reduction; further evidence includes the presence of C-13-depleted calcite cements (similar to-12 parts per thousand delta(13)C) as sulfate pseudomorphs, elemental sulfur, altered organic matter in the host dolomite, and isotopically heavier, late, solid bitumen. Significant alteration of the indigenous and extrinsic hydrocarbons, with absent bacterial membrane biomarkers (hopanes) is observed. The light delta(34)S of sulfides from small mines and occurrences compared to the main deposit reflect a local contribution of isotopically light sulfur, evidence of local differences in the ore-fluid chemistry.