162,796 research outputs found
Y-specific microsatellites reveal an African subfamily in taurine (Bos taurus) cattle
No full textPérez-Pardal, L., Royo, L.J., Beja-Pereira, A., Curik, I., Traoré, A., Fernández, I., Sölkner, J., Alonso, J., Álvarez, I., Bozzi, R., Chen, S., Ponce De León, F.A., Goyache, F
Trolliet (P.), Beja (J.-Ph.). — L'Empire du milliard. Collection U. 1986
No full textLerat Serge. Trolliet (P.), Beja (J.-Ph.). — L'Empire du milliard. Collection U. 1986. In: Cahiers d'outre-mer. N° 157 - 40e année, Janvier-mars 1987. p. 80
J. Marcadé, Freí Manuel do Cenáculo Vilas Boas, évêque de Beja, archevêque d'Evora (1770-1814)
No full textRicard Robert. J. Marcadé, Freí Manuel do Cenáculo Vilas Boas, évêque de Beja, archevêque d'Evora (1770-1814). In: Bulletin Hispanique, tome 80, n°3-4, 1978. pp. 320-324
[Report to Chief J. E. Curry, by an unknown author #1]
No full textReport to Chief J. E. Curry, by an unknown author. The report contains a list of officers who gave depositions to the United States Attorney
[Report to Chief J. E. Curry, by an unknown author #2]
No full textReport to Chief J. E. Curry, by an unknown author. The report contains a list of officers who gave depositions to the United States Attorney
Murder on the mountain: author talk with Peter J. Wosh
No full textAuthor talk by Peter J. Wosh on May 5th, 2022, on his book, "Murder on the Mountain: crime, passion, and punishment in gilded age New Jersey.
Mr. Melvin J. Collier, RWWL AUC, June 2011
No full textThis video is a conversation with Mr. Melvin J. Collier. Mr. Collier talks about his book, "From Mississippi to Africa: A Journey of Discovery". Daniel Le, AUC Woodruff Library, is the interviewer
A Tripartite Post-Recession Rebalancing
No full textIn this latest Advance & Rutgers Report, entitled “A Tripartite Post-Recession Rebalancing,” Dean James W. Hughes and Professor Joseph J. Seneca deliver an incisive assessment of the current market conditions and obstacles in the path of our economic recovery. They offer a statistical cautionary tale that the private and public sector need to hear and acknowledge in order for the economy to make continued progress.This report was published as Issue Paper Number 7, November 2011, in Advance & Rutgers Report
Evidence for the decay B0→J/ψω and measurement of the relative branching fractions of meson decays to J/ψη and J/ψη′
No full textFirst evidence of the B 0 → J / ψ ω decay is found and the B s 0 → J / ψ η and B s 0 → J / ψ η ′ decays are studied using a dataset corresponding to an integrated luminosity of 1.0 fb -1 collected by the LHCb experiment in proton-proton collisions at a centre-of-mass energy of sqrt(s) = 7 TeV. The branching fractions of these decays are measured relative to that of the B 0 → J / ψ ρ 0 decay:frac(B (B 0 → J / ψ ω), B (B 0 → J / ψ ρ 0)) = 0.89 ± 0.19 (stat) - 0.13 + 0.07 (syst),frac(B (B s 0 → J / ψ η), B (B 0 → J / ψ ρ 0)) = 14.0 ± 1.2 (stat) - 1.5 + 1.1 (syst) - 1.0 + 1.1 (frac(f d, f s)),frac(B (B s 0 → J / ψ η ′), B (B 0 → J / ψ ρ 0)) = 12.7 ± 1.1 (stat) - 1.3 + 0.5 (syst) - 0.9 + 1.0 (frac(f d, f s)), where the last uncertainty is due to the knowledge of f d / f s, the ratio of b-quark hadronization factors that accounts for the different production rate of B 0 and B s 0 mesons. The ratio of the branching fractions of B s 0 → J / ψ η ′ and B s 0 → J / ψ η decays is measured to befrac(B (B s 0 → J / ψ η ′), B (B s 0 → J / ψ η)) = 0.90 ± 0.09 (stat) - 0.02 + 0.06 (syst)
Trigaches Marbles (São Brissos, Beja, Portugal): petrographic and geochemical characterization of a historical dimension stone
No full textThe exploitation of carbonate crystalline rocks in the Ossa-Morena Zone (OMZ) dates back more than two thousand years. Several historical exploitation poles in OMZ were identified based on the identification of distinctive marble lithotypes in Roman consumption areas, and some of those historical exploitation places were, subsequently, identified in situ through geo-archaeological works (e.g. Almadén de la Plata, Estremoz Anticline). The distinctive macroscopic features of Trigaches Marbles also allowed to recognize their use on Roman architecture, but also in several buildings, namely in southern Portugal, along numerous historical periods until present days, which indicates a long lived history of exploitation of this dimension stone. The Trigaches Marbles are exploited in Trigaches - São Brissos parish (Beja, Alentejo), located at the SW border of the OMZ. The geological unit containing the Trigaches Marbles has been assigned to Cambrian (as most of the exploited marbles on OMZ), outcropping in a N-S elongated strip with approximately 1.5 km2 of area. This unit contacts with Carboniferous magmatic bodies to the west and north, and with a predominantly metasedimentary unit, composed of schists and subordinate metavolcanic rocks, to the east.
At macroscopic scale, Trigaches Marbles can be light grey, dark grey or grey-scale banded marbles, showing a poorly developed subvertical to steeply dipping metamorphic banding, subparallel to the main unit trend. Marbles are mainly composed of calcite (generally above 97% of volume - just one sample has a proportion around 95%), exhibiting a well-developed non-oriented granoblastic texture, commonly with tendency towards polygonization of calcite grains. As minor mineral phases, quartz, opaque minerals, biotite or muscovite, and sporadically, scapolite and pyroxene were identified. Marbles are inequigranular, generally coarse to very coarse grained, although sometimes medium grained calcite is also present (grain size ranges from 0.5mm to 20-40 mm). Calcite crystals commonly present type 4 twins, indicating medium-high temperature recrystallization, in accordance with the grain size.
Major element geochemical data show great homogeneity, in accordance with mineral modal composition: CaO ranges between 52.2 and 54.8% whilst MgO varies from 0.4 to 1.0%, in accordance with the calcite nature of these marbles and the absence of dolomite; low concentrations of Al2O3 [0.8 - 0.1%], K2O [0.0 - 0.2%] and Na2O [0.0 - 0.3%] agree with low phyllosilicate contents and the absence of feldspars s.l.; SiO2 can reach 2% of whole rock being related mostly to the presence of quartz (can reach 3% of modal composition); LOI range between 42.5 and 43.9%, mainly indicative of the CO2 content.publishe
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