1.° Caii Plinii Secundi epistolarum libri decem : primi initium et decimi finis desiderantur. — 2.° Ejusdem panegyricus Trajano dictus. — 3.° Latini Pacati Drepanii panegyricus Theodosio dictus. — 4.° Claudii Mamertini Juliano Imperatori gratiarum actio de Consulatu suo. — 5.° Nazarii panegyricus Constantino, Caesari, dictus. — 6.° Eumenii gratiarum actio Constantino, Augusto, Flaviensium nomine. — 7.° Ejusdem panegyricus Constantino, Augusto, dictus. — 8.° Incerti authoris panegyricus Maximiano et Constantino dictus. — 9.° Eumenii panegyricus Constantio, Caesari, dictus. — 10.° Ejusdem oratio pro restaurandis scholis. — 11.° Claudii Mamertini panegyricus Maximiano, Augusto, dictus. — 12.° Genethliacus Maximiani : authore eodem. — 13.° Incerti authoris panegyricus Constantino, Augusto, dictus : finis desideratur.

Bigotianus

Modelling changes in stable isotope compositions of minerals during net transfer reactions in a contact aureole: Wollastonite growth at the northern Hunter Mountain Batholith (Death Valley National Park, USA)

One of the world's largest wollastonite deposits was formed at the contact of the northern Hunter Mountain Batholith (California, USA) in Paleozoic sediments. Wollastonite occurs as zones of variable thickness surrounding layers or nodules of quartzite in limestones. A minimum formation temperature of 650 degrees C is estimated from isolated periclase-bearing lenses in that area. Contact metamorphism of siliceous carbonates has produced mineral assemblages that are consistent with heterogeneous, and partly limited infiltration of water-rich fluids, compatible with O-18/O-16 and C-13/C-12 isotopic patterns recorded in carbonates. Oxygen isotope compositions of wollastonites in the study area may also not require infiltration of large quantities of externally-derived fluids that were out of equilibrium with the rocks. 8180 values of wollastonite are high (14.8 parts per thousand to 25.0 parts per thousand; median: 19.7 parts per thousand) and close to those of the host limestone (19.7 parts per thousand to 28 parts per thousand; median: 24.9 parts per thousand) and quartz (18.0 parts per thousand. to 29.1 parts per thousand; median: 22.6 parts per thousand). Isotopic disequilibrium exists at quartz/wollastonite and wollastonite/calcite boundaries. Therefore, classical batch/Rayleigh fractionation models based on reactant and product equilibrium are not applicable to the wollastonite rims. An approach that relies on local instantaneous mass balance for the reactants, based on the wollastonite-forming reaction is suggested as an alternative way to model wollastonite reaction rims. This model reproduces many of the measured delta O-18 values of wollastonite reaction rims of the current study to within +/- 1 parts per thousand, even though the wollastonite compositions vary by almost 10 parts per thousand. (C) 2011 Elsevier B.V. All rights reserved.

13/11/19, affiches électorales [panneaux électoraux dans la rue pour les élections législatives du 16 novembre 1919] : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 56908

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13-12-19, stade Jean-Bouin, hockey [sur gazon], équipe des Possibles : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 57224