[4 phot. des monuments élevés par Jean Joseph de La Borde dans le parc de son château de Méréville (Seine-et-Oise), à la fin du XVIIIe siècle, à la mémoire de ses deux fils, de La Borde-Marchainville et de La Borde-Boutervilliers, officiers de l'Astrolabe, péris avec La Pérouse en 1786, ainsi qu'à la mémoire du capitaine Cook, don du prince Roland Bonaparte en 1896. Voir les CR. des séances de la S.G., 1896, p. 319-321]

Donateur : Bonaparte, Roland (1858-1924)

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.

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.