Diário da Constituinte [gravação de vídeo] : [programa n. 106]

A Comissão de Organização dos Estados da Assembleia Nacional Constituinte (ANC) propôs nas disposições transitórias a criação de novos estados: Tapajós; Triângulo; Santa Cruz; Maranhão do Sul e Tocantins. Também foi aprovada a transformação dos territórios de Roraima e Amapá em estados. Chagas Duarte (PFL-RR) quer transformar o território de Roraima em estado. Marluce Pinto (PTB-RR) afirma que o que falta em Roraima é a criação de uma Assembleia Legislativa. Reunião da Liderança do PMDB discute temas conflitantes entre os relatórios das várias comissões da Constituinte. Os demais líderes partidários serão consultados posteriormente. Biografia dos relatores adjuntos: Wilson Martins (PMDB-MS), José Ignácio Ferreira (PMDB-ES), Nelson Jobim (PMDB-RS) e Fernando Henrique Cardoso (PMDB-SP).

Fernando del Pulgar y la vejez

[ES]Aproximación a la consideración social de los ancianos a finales de la Edad Media y cómo ellos vivían su situación a través del ejemplo del cronista Fernando del Pulgar (Castilla siglo XV).

Divinidades y devotos indígenas en la "Tarraconensis": las dedicaciones colectivas

Presentado en: Acta Paleohispanica X. Actas do X Colóquio Internacional sobre Línguas e Culturas Paleo-Hispânicas. Lisboa, 26-28 de Fevereiro de 2009

Observaciones sobre la fórmula "in hono. Argael." en un epígrafe de Cacabelos, León (CIL II 5672)

Ejemplar dedicado a: Serta Palaeohispanica in honorem Javier de Hoz

Sobre la "religio" de los pueblos del NW durante el alto imperio: algunas observaciones

Presentado en: Acta Palaeohispanica, IX. Actas del IX Coloquio sobre Lenguas y Culturas Palaeohispánicas. Barcelona, 20-24 de octubre de 2004

Ictiólogos de la Argentina: Fernando Lahille.

This series will include all those people who, by means of their contributions, great and small, played a part in the consolidation of ichthyology in Argentina. The general plan of this work consists of individual factsheets containing a list of works by each author, along with reference bibliography and, whenever possible, personal pictures and additional material. The datasheets will be published primarily in chronological order, although this is subject to change by the availability of materials for successive editions. This work represents another approach for the recovery and revalorization of those who set the foundations of Argentine ichthyology while in diverse historical circumstances. I expect this to be the beginning of a major work that achieves the description of such a significant part of the history of natural sciences in Argentina. Hugo L. López (Texto en espanol. PDF tiene setenta y dos paginas.)

Fernando Lahille. Ictiólogo.

Breve reseña histórica de la actividad ictiológica de Fernando Lahille.

Histoire de la Province de Sancta-Cruz, que nous nommons ordinairement le Brésil

Dédié au très-illustre seigneur D. Lionis Pereira

Tratado de limites das conquistas entre os muito altos, e poderosos senhores D. João V, Rey de Portugal, e D. Fernando VI, Rey de Espanha, pelo qual abolida a demarcação da linha meridiana, ajustada no Tratado de Tordesilhas de 7 de junho de 1494, se determina individualmente a raya dos domínios de huma e outra corôa na America Meridional :a de Portugal renuncia o direito, que allegava ter das Ilhas Filippinas, pelo dito Tratado de Tordesilhas, e pela escritura de Saragoça de 22 de abril de 1529 ; e cede a Espanha a Colonia do Sacramento, e o Territorio da margem septentrional do Rio da Prata, que lhe pertencia pelo Tratado de Utrecht de 6 de fevereiro de 1715, como também a Aldea de S. Christóvão, e terras adjacentes, que tinhão occupado os portuguezes entre os rios Japurá, e Isa, que desaguão no das Amazonas; a de Espanha renuncia todo o direito, que pelo dito Tratado de Tordesilhas allegava ter as terras possuidas pelos portuguezes na America Meridional ao Occidente da Linha Meridiana, ajustada naquelle Tratado ; e cede a Portugal todas as terras, e povoações da margem oriental do rio Uruguay, desde o rio Ibicuí para o norte, e a aldea de Santa Rosa, e outra qualquer estabelecida pelos espanhoes na margem oriental do rio Guaporé; com os plenos-poderes, e ratificações dos dous Monarchas, assignado em Madrid a 13 de janeiro de 1750

Referência: Diccionario Bibliographico Portuguez / Innocencio Francisco da Silva, 1862. v. 7, p. 386.

Analysis of SUMOylated proteins using SUMO-traps

6 p. [+ 7 p. Supplementary Information]

Cartas enviadas por Rodolfo Armas Cruz a Justo Garate en 1965

2 cartas (mecanografiadas) ; 210x268mm. Ubicación: Caja 1 - Carpeta 52

Síntese do rito processual seguido no Impeachment do Presidente Fernando Collor de Mello

Sintetiza os procedimentos levados a efeito no âmbito da Câmara dos Deputados e do Senado Federal, quando do processo de Impeachment contra o Presidente Fernando Collor de Mello, em 1992.

Part I. A study of the velocity structure of the earth by the use of core phases. Part II. The 1971 San Fernando earthquake series focal mechanisms and tectonics

The initial objective of Part I was to determine the nature of upper mantle discontinuities, the average velocities through the mantle, and differences between mantle structure under continents and oceans by the use of P'dP', the seismic core phase P'P' (PKPPKP) that reflects at depth d in the mantle. In order to accomplish this, it was found necessary to also investigate core phases themselves and their inferences on core structure. P'dP' at both single stations and at the LASA array in Montana indicates that the following zones are candidates for discontinuities with varying degrees of confidence: 800-950 km, weak; 630-670 km, strongest; 500-600 km, strong but interpretation in doubt; 350-415 km, fair; 280-300 km, strong, varying in depth; 100-200 km, strong, varying in depth, may be the bottom of the low-velocity zone. It is estimated that a single station cannot easily discriminate between asymmetric P'P' and P'dP' for lead times of about 30 sec from the main P'P' phase, but the LASA array reduces this uncertainty range to less than 10 sec. The problems of scatter of P'P' main-phase times, mainly due to asymmetric P'P', incorrect identification of the branch, and lack of the proper velocity structure at the velocity point, are avoided and the analysis shows that one-way travel of P waves through oceanic mantle is delayed by 0.65 to 0.95 sec relative to United States mid-continental mantle.

A new P-wave velocity core model is constructed from observed times, dt/dΔ's, and relative amplitudes of P'; the observed times of SKS, SKKS, and PKiKP; and a new mantle-velocity determination by Jordan and Anderson. The new core model is smooth except for a discontinuity at the inner-core boundary determined to be at a radius of 1215 km. Short-period amplitude data do not require the inner core Q to be significantly lower than that of the outer core. Several lines of evidence show that most, if not all, of the arrivals preceding the DF branch of P' at distances shorter than 143° are due to scattering as proposed by Haddon and not due to spherically symmetric discontinuities just above the inner core as previously believed. Calculation of the travel-time distribution of scattered phases and comparison with published data show that the strongest scattering takes place at or near the core-mantle boundary close to the seismic station.

In Part II, the largest events in the San Fernando earthquake series, initiated by the main shock at 14 00 41.8 GMT on February 9, 1971, were chosen for analysis from the first three months of activity, 87 events in all. The initial rupture location coincides with the lower, northernmost edge of the main north-dipping thrust fault and the aftershock distribution. The best focal mechanism fit to the main shock P-wave first motions constrains the fault plane parameters to: strike, N 67° (± 6°) W; dip, 52° (± 3°) NE; rake, 72° (67°-95°) left lateral. Focal mechanisms of the aftershocks clearly outline a downstep of the western edge of the main thrust fault surface along a northeast-trending flexure. Faulting on this downstep is left-lateral strike-slip and dominates the strain release of the aftershock series, which indicates that the downstep limited the main event rupture on the west. The main thrust fault surface dips at about 35° to the northeast at shallow depths and probably steepens to 50° below a depth of 8 km. This steep dip at depth is a characteristic of other thrust faults in the Transverse Ranges and indicates the presence at depth of laterally-varying vertical forces that are probably due to buckling or overriding that causes some upward redirection of a dominant north-south horizontal compression. Two sets of events exhibit normal dip-slip motion with shallow hypocenters and correlate with areas of ground subsidence deduced from gravity data. Several lines of evidence indicate that a horizontal compressional stress in a north or north-northwest direction was added to the stresses in the aftershock area 12 days after the main shock. After this change, events were contained in bursts along the downstep and sequencing within the bursts provides evidence for an earthquake-triggering phenomenon that propagates with speeds of 5 to 15 km/day. Seismicity before the San Fernando series and the mapped structure of the area suggest that the downstep of the main fault surface is not a localized discontinuity but is part of a zone of weakness extending from Point Dume, near Malibu, to Palmdale on the San Andreas fault. This zone is interpreted as a decoupling boundary between crustal blocks that permits them to deform separately in the prevalent crustal-shortening mode of the Transverse Ranges region.