[Voyage en Italie : 1824-1830]. , Monastère du Mont-Cassin à S. Germano (royaume de Naples). Bâti par Fonzago architecte 1649 : [plan moderne] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 65

[Voyage en Italie : 1824-1830]. , Abbaye du Mont-Cassin à S. Germano : [vue perspective] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 66

[Voyage en Italie : 1824-1830]. , [Abbaye du ] Mont-Cassin : [vue perspective d'une cour] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 67

Intrinsic coordinate system for the tibial plateau

Determination of the sub-chondral bone density, or more precisely the internal density spot, can be used to evaluate the capability of a knee to sustain normal kinematics. To use this technique as a mean of knee kinematics control, the position of the internal density spot must be determined in a reproducible way. This paper presents a definition of an intrinsic polar coordinate system, allowing to measure the position of the internal density spot of the tibial plateau. Tests of reproducibility gave good results and justify the use of this coordinate system for comparison of the internal density spot position between left and right paired knees.

[Voyage en Italie : 1824-1830]. , Entrée de la maison Pansa : [vue perspective avec un péristyle au second plan et le mont Vésuve en arrière-plan] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 401

L' arrest du Conseil d'en-haut, prononcé par le prophete royal David, contre Mazarin & les partisans. Par F.A.S.D.R.

[Mazarinade. 1649]

A Variscan pressure-temperature-time path for the N-E Mont Blanc massif

The northeastern portion of the Mont Blanc massif in western Switzerland is predominantly comprised of the granitic rocks of the Mont Blanc intrusive suit, and the Mont Blanc basement gneisses. Within these metamorphic rocks are a variety of sub-economic Fe skarns. The mineral assemblages and fluid inclusions from these rocks have been used to derive age, pressure, temperature and fluid composition constraints for two Variscan events. Metamorphic hornblendes within the assemblages from the basement amphibolites and iron sk:lms have been dated using Ar-40/Ar-39, and indicate that these metamorphic events have a minimum age of approximately 334 Ma. Garnet-hornblende-plagioclase thermobarometry and stable isotope data obtained from the basement amphibolites are consistent with metamorphic temperatures in the range 515 to 580 degrees C, and pressures ranging from 5 to 8 kbar. Garnet-hornblende-magnetite thermobarometry and fluid inclusion studies indicate that the iron skarns formed at slightly lower temperatures, ranging from 400 to 500 degrees C in the presence of saline fluids at formational pressures similar to those experienced by the basement amphibolites. Late Paleozoic minimum uplift rates and geothermal gradients calculated using these data and the presence of Ladinien ichnofossils are on the order of 0.32 mm/year and 20 degrees C/km respectively. These uplift rates and geothermal gradients differ from those obtained from the neighbouring Aiguilles Rouges massif and indicate that these two massifs experienced different metamorphic conditions during the Carboniferous and Permian periods. During the early to late Carboniferous period the relative depths of the two massifs were reversed with the Aiguilles Rouges being initially unroofed at a much greater rate than the Mont Blanc, but experiencing relatively slower uplift rates near the termination of the Variscan orogeny.

Basilikon dōron, ou Présent royal de Jaques premier, roy d'Angleterre, Escoce et Irlande, au prince Henry, son fils, contenant une instruction de bien régner . Traduit de l'anglois.

Titre original : His Majesties instructions to his dearest sonne, Henry the prince

Apport du CT-3D dans le diagnostic et le traitement des fractures des plateaux tibiaux [Value of 3D CT in diagnosis and treatment of fractures of the tibial plateau]

A precise classification and an optimal understanding of tibial plateau fractures are the basis of a conservative treatment or adequate surgery. The aim of this prospective study is to determine the contribution of 3D CT to the classification of fractures (comparison with standard X-rays) and as an aid to the surgeon in preoperative planning and surgical reconstruction. Between November 1994 and July 1996, 20 patients presenting 22 tibial plateau fractures were considered in this study. They all underwent surgical treatment. The fractures were classified according to the Müller AO classification. They were all investigated by means of standard X-rays (AP, profile, oblique) and the 3D CT. Analysis of the results has shown the superiority of 3D CT in the planning (easier and more acute), in the classification (more precise), and in the exact assessment of the lesions (quantity of fragments); thereby proving to be of undeniable value of the surgeon.