Suite from L'histoire du soldat, for clarinet, violin and piano,

Mode of access: Internet.

Also sprach Zarathustra : Tondichtung, frei nach Friedr. Nietzsche, für grosses Orchester, Op. 30 /

Originally for orchestra; arr. for 2 pianos, 4 hands.

Indian suite /

For piano, 2 hands.

La folia. [music] : variations sérieuses pour le violin /

Stamped on t.p.: Sole agents: C. F. Peters Corp., New York, N.Y.

Hungarian dances : nos. 1, 3, 10 /

Mode of access: Internet.

Anatomical landmarks for transnasal endoscopic skull base surgery.

Resection of midline skull base lesions involve approaches needing extensive neurovascular manipulation. Transnasal endoscopic approach (TEA) is minimally invasive and ideal for certain selected lesions of the anterior skull base. A thorough knowledge of endonasal endoscopic anatomy is essential to be well versed with its surgical applications and this is possible only by dedicated cadaveric dissections. The goal in this study was to understand endoscopic anatomy of the orbital apex, petrous apex and the pterygopalatine fossa. Six cadaveric heads (3 injected and 3 non injected) and 12 sides, were dissected using a TEA outlining systematically, the steps of surgical dissection and the landmarks encountered. Dissection done by the "2 nostril, 4 hands" technique, allows better transnasal instrumentation with two surgeons working in unison with each other. The main surgical landmarks for the orbital apex are the carotid artery protuberance in the lateral sphenoid wall, optic nerve canal, lateral optico-carotid recess, optic strut and the V2 nerve. Orbital apex includes structures passing through the superior and inferior orbital fissure and the optic nerve canal. Vidian nerve canal and the V2 are important landmarks for the petrous apex. Identification of the sphenopalatine artery, V2 and foramen rotundum are important during dissection of the pterygopalatine fossa. In conclusion, the major potential advantage of TEA to the skull base is that it provides a direct anatomical route to the lesion without traversing any major neurovascular structures, as against the open transcranial approaches which involve more neurovascular manipulation and brain retraction. Obviously, these approaches require close cooperation and collaboration between otorhinolaryngologists and neurosurgeons.

Shostakovich i el violí : el Concert per a violí núm. 1 op. 77 i els Preludis op. 34

L’objectiu del projecte final titulat Shostakovich i el violí és l’estudi de la vida, el context històric i l’obra del cèlebre compositor rus Dmitri Shostakovich, parant una especial atenció en dues de les seves composicions: el Concert per a violí núm. 1 opus 77 i els Preludis per a piano opus 34 (arranjats per a violí i piano per Dmitri Tsyganov). La metodologia usada en l’elaboració del treball ha consistit en la recerca d’informació a través de biografies de Shostakovich, reculls de les seves memòries, records de persones pròximes al compositor, articles i cartes publicades per ell, així com estudis o anàlisis de les seves obres musicals. La conclusió extreta és que l’obra de Shostakovich està íntimament lligada amb el context històric en el qual va viure, és a dir, amb la seva època, tal com es pot apreciar tant en la seva escriptura com en el contingut emocional de les seves obres.

Two-stage prograde and retrograde Variscan metamorphism of glaucophane-eclogites, blueschists and greenschists from Ile de Groix (Brittany, France)

On Ile de Groix, Variscan metamorphic former tholeiitic and alkaline basalts occur as glaucophane-eclogites, blueschists and greenschists in isolated lenses and layers within metapelites. Whole-rock delta O-18(SMOW) values of the metabasites show limited variations (10.4-12.0 parts per thousand) and no systematic differences among rock types and metamorphic grades. This provides no argument for large-scale blueschist-to-greenschist transformation driven by infiltration of externally derived fluids. Metamorphic mineralogical changes should have been triggered by internal fluids. Element variations in interlayered blue- and greenschists can be attributed to magmatic fractionation. Assemblages with garnet, clinopyroxene and glaucophane of a high-pressure/low-temperature (HP-LT) metamorphism M1, and NaCa-amphiboles (barroisite, magnesiohornblende, actinolite) of a medium-pressure/medium-temperature metamorphism M2 crystallized during deformation Dl. Detailed core-rim zonation profiles display increasing and then decreasing Al-IV in glaucophane of M1. NaCa-amphiboles of M2, mantling glaucophane and crystallized in porphyroblasts, show first increasing, then decreasing, Al-IV and Al-IV. Empirically calibrated thermobarometers allowed P-T path reconstructions. In glaucophane-eclogites of a metamorphic zone I, a prograde evolution to M1 peak conditions at 400-500 degreesC/10-12 kbar was followed by a retrograde P-T path within the glaucophane stability field. The subsequent M2 evolution was again prograde up to > 600 degreesC at 8 kbar and then retrograde. Similarly, in metamorphic zones II and III, prograde and retrograde paths of MI and M2 at lower maximal temperatures and pressures exist. The almost complete metamorphic cycle during M2 signalizes that the HP-LT rocks escaped from an early erosion by a moderate second burial event and explains the longlasting slow uplift with low average cooling rates.

Respolska

Soitinnus: piano, 4-kät.

Symfoni III

Mukana myös kaksi keskeneräistä 4-kätistä pianosovitusta I osasta, vanhempi versio II osasta, keskeneräinen versio II osasta sekä II osan orkesteristemmat.

Six epigraphes antiques

Soitinnus : Piano, 4-kät.

Intermezzo humoristica

Soitinnus: piano, 4-kät.

Tranquillo

Soitinnus: piano, 4-kät.

Marionettes

Soitinnus: piano, 4-kät.