Szenenfoto: Richard Strauss: Ariadne auf Naxos

Signatur des Originals: S 36/F07628

{[N.N.], Szenenfoto, Gruppenbildnis, in: Richard Strauss: Ariadne auf Naxos, München

Signatur des Originals: S 36/F07724

{[N.N.], Szenenfoto, Gruppenbildnis, in: Richard Strauss: Ariadne auf Naxos, München

Signatur des Originals: S 36/F07725

Schneider-Scene i. "Ariadne auf Naxos"

Signatur des Originals: S 36/F07726

Schneider-Scene i. "Ariadne auf Naxos"

Signatur des Originals: S 36/F07727

Schneider-Scene i. "Ariadne auf Naxos"

Signatur des Originals: S 36/F07729

{[N.N.], Szenenfoto, in: Richard Strauss: Ariadne auf Naxos, München

Signatur des Originals: S 36/F07728

{[N.N.], Szenenfoto, Gruppenbildnis, in: Richard Strauss: Ariadne auf Naxos

Signatur des Originals: S 36/F12181

Le Temple de Bacchus dans l'Isle de Naxos

Signatur des Originals: S 36/G13802

Campagne et bocage agreable dans l'Isle de Naxos

Signatur des Originals: S 36/G03816

Dorfmusik auf den Cycladen, Tracht der Bewohner der Insel Naxos

Signatur des Originals: S 36/G04504

Vue perspective du Grand Cabinet du Lauriers dans les jardins du Roy de l'Isle de Naxos c'est la derniere Décoration du 3.me acte, et de tout l'Opera de Venus jalouse repre.té a Venise

Signatur des Originals: S 36/G04529

Ariadne auf Naxos : ... Duodrama mit der vortreflichen Musik des Herrn Benda ... ; alsdann folgt Der Edelknabe ; ein Lustspiel in einem Aufzuge von Herrn Engel ; den Beschluß macht ein groses tragisches von Hrn. Vogt nach Angiolini verfertigtes Ballet in fünf Aufzügen, genannt Don Juan, oder der steinerne Gast ; 4. Mai 1782 ; im neuerbauten Comödien-Haus im Junghof ; [Theaterzettel]

Schauspieler-Gesellschaft unter der Direction des Herrn Böhm

Naxos siceliota; storia, topografia, avanzi, monete.

Mode of access: Internet.

Coaxial flattening at deep levels of orogenic belts: evidence from blueschists and eclogites on Syros and Sifnos (Cyclades, Greece)

This work presents new Structural data from a high-pressure/low-temperature (HP/LT) metamorphic terrane exposed on the islands of Syros and Sifnos (Cyclades, Greece). The structure and the metamorphism of a relatively coherent HP/LT rock section were studied in order to elucidate how strain was accommodated at deep crustal levels during the formation and exhumation of HP/LT rocks. At least three deformation phases associated with eclogite- and blueschist-facies conditions (P = 8-15 kbar; T = 400-550 degreesC) were recognised. The earliest deformation fabric (S1), preserved as inclusion trails within garnet porphyroblasts, is aligned to define a sub-vertical schistosity (at present orientation), which is frequently orthogonal to the flat matrix schistosity (S2), and may indicate that deep crustal thickening involved upright folding. The currently dominant fabric in the HP rock section, S2, is Usually moderately dipping and locally contains NW-trending glaucophane lineations, symmetric pressure-shadows and eclogitic boudins. The symmetric structures associated with this fabric seem to indicate coaxial vertical thinning, although the existence of non-coaxial structures out of the study area cannot be excluded. Glaucophane-bearing shear bands (S3), with top-to-NW sense of shearing, locally crosscut the earlier structures. The latest recognised fabric (D4) is scarce and often absent within the HP rocks. It is associated with top-to-NE kinematic criteria that formed at greenschist-facies conditions (P = 4-7 kbar; T = 400-450 degreesC). Based on these observations, it is suggested that partitioning of strain occurred at different crustal levels and at different times. Deep crustal deformation was governed by thickening via upright folding followed by coaxial vertical thinning, whereas non-coaxial shearing occurred when the rocks were already exhumed to relatively shallow crustal levels. The earliest fabrics (D1 to D3) pertain to Alpine orogenesis and possibly to syn-orogenic extension, whereas the latest correspond to whole-crust back-are extension. (C) 2002 Elsevier Science Ltd. All rights reserved.