324,415 research outputs found
Wunder und Wundergeschichten
No full textWunder und Wundergeschichten. - In: Modelle für den Religionsunterricht in der Sekundarstufe I / Günther Staudigl ... (Hrsg.). - Donauwörth : Auer, 1977. - S. 170-176. - (Reihe Exempla ; 20
Wunder, Dieter (Hrsg.): Ein neuer Beruf? - Lehrerinnen und Lehrer an Ganztagsschulen. Wochenschau Verlag, Schwalbach/Ts. 2008, 140 S. [Rezension]
No full textRezension zu: Wunder, Dieter (Hrsg.): Ein neuer Beruf? – Lehrerinnen und Lehrer an Ganztagsschulen. Wochenschau Verlag, Schwalbach/Ts. 2008, 140 S., ISBN 978-3-89974206-
S. Scharinger, Die Wunder des Pythagoras
No full textDiese Monographie ist die überarbeitete Fassung einer Dissertation, die im Wintersemester 2016-2017 am Institut für Alte Geschichte und Altorientalistik der Philosophisch-Historischen Fakultät der Leopold-Franzens-Universität Innsbruck mit dem Titel „Wunderbares aus dem Leben des Pythagoras von Samos im Vergleich“ eingereicht wurde
Diffusive author(s), cohesive author: Analysis of S/N (1994)
No full textThis study indicates the ways in which various aspects of the author(s) are brought forth in Dumb type’s performance art, the S/N production. Previous research has suggested a non-hierarchical organization of Dumb type and the absence of a “privileged author” in Dumb type’s collaborative work, S/N. However, the results that I have investigated from member’s interviews on the creative process of S/N along with my analysis of the recorded images of S/N, indicate a different aspect of the author(s). First, S/N was created through, so to speak, the collective ideas of the members of Dumb type. Further, S/N has at least nine quotations from previous performances, installations, and printed writings, besides the work-in-progress technique. Explicating one of the “author functions” as given by Michel Foucault, each text has plural subjects of the author. However, it has been revealed from members’ interviews that Teiji Furuhashi had a decision-making role in selecting the members’ ideas within the performance. Since then, S/N has had plural subjects of creation; however, Furuhashi is one of the subjects of creation along with the “privileged author.” S/N has plural authors (diffusive authors) yet at the same time, it has a “privileged author,” Teiji Furuhashi (cohesive author)
Partial melting of ultramafic granulites from Dronning Maud Land, Antarctica: Constraints from melt inclusions and thermodynamic modeling
No full textIn the Pan-African belt of the Dronning Maud Land, Antarctica, crystallized melt inclusions (nano-granitoids) occur in garnet from ultramafic granulites. The granulites contain the peak assemblage pargasite+garnet+clinopyroxene with rare relict orthopyroxene and biotite, and retrograde symplectites at contacts between garnet and amphibole. Garnet contains two generations of melt inclusions. Type 1 inclusions, interpreted as primary, are isolated, <10 μm in size, and generally have negative crystal shapes. They contain kokchetavite, kumdykolite, and phlogopite, with quartz and zoisite as minor phases, and undevitrified glass was identified in one inclusion. Type 2 inclusions are <30 μm in size, secondary, and contain amphibole, feldspars, and zoisite. Type 2 inclusions appear to be the crystallization products of a melt that coexisted with an immiscible CO2-rich fluid. The nanogranitoids were re-homogenized after heating in a piston-cylinder in a series of four experiments to investigate their composition. The conditions ranged between 900 and 950 °C at 1.5-2.4 GPa. Type 1 inclusions are trachytic and ultrapotassic, whereas type 2 melts are dacitic to rhyolitic. Thermodynamic modeling of the ultramafic composition in the MnNCKFMASHTO system shows that anatexis occurred at the end of the prograde P-T path, between the solidus (at ca. 860 °C-1.4 GPa) and the peak conditions (at ca. 960 °C-1.7 GPa). The model melt composition is felsic and similar to that of type 1 inclusions, particularly when the melting degree is low (<1 mol%), close to the solidus. However the modeling fails to reproduce the highly potassic signature of the melt and its low H2O content. The combination of petrology, melt inclusion study, and thermodynamic modeling supports the interpretation that melt was produced by anatexis of the ultramafic boudins near peak P-T conditions, and that type 1 inclusions contain the anatectic melt that was present during garnet growth. The felsic, ultrapotassic composition of the primary anatectic melts is compatible with low melting degrees in the presence of biotite and amphibole as reactants
Going Beyond Counting First Authors in Author Co-citation Analysis
No full textThe present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation
counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings
are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that
only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into
account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed
Neuer Geist aus religiöser Tiefe: wie das "Wunder von Trient " die Kirche reformierte
No full textNeuer Geist aus religiöser Tiefe : wie d. "Wunder von Trient " d. Kirche reformierte. - In: Der Fels. 27. 1996. 1. S. 8-1
Partial melting of ultramafic granulites from Dronning Maud Land, Antarctica: Constraints from melt inclusions and thermodynamic modeling
No full textIn the Pan-African belt of the Dronning Maud Land, Antarctica, crystallized melt inclusions (nanogranitoids) occur in garnet from ultramafic granulites. The granulites contain the peak assemblage pargasite+garnet+clinopyroxene with rare relict orthopyroxene and biotite, and retrograde symplectites at contacts between garnet and amphibole. Garnet contains two generations of melt inclusions. Type 1 inclusions, interpreted as primary, are isolated, < 10 mu m in size, and generally have negative crystal shapes. They contain kokchetavite, kumdykolite, and phlogopite, with quartz and zoisite as minor phases, and undevitrified glass was identified in one inclusion. Type 2 inclusions are < 30 mu m in size, secondary, and contain amphibole, feldspars, and zoisite. Type 2 inclusions appear to be the crystallization products of a melt that coexisted with an immiscible CO2-rich fluid.
The nanogranitoids were re-homogenized after heating in a piston-cylinder in a series of four experiments to investigate their composition. The conditions ranged between 900 and 950 degrees C at 1.5-2.4 GPa. Type 1 inclusions are trachytic and ultrapotassic, whereas type 2 melts are dacitic to rhyolitic. Thermodynamic modeling of the ultramafic composition in the MnNCKFMASHTO system shows that anatexis occurred at the end of the prograde P-T path, between the solidus (at ca. 860 degrees C-1.4 GPa) and the peak conditions (at ca. 960 degrees C-1.7 GPa). The model melt composition is felsic and similar to that of type 1 inclusions, particularly when the melting degree is low (< 1 mol%), close to the solidus. However the modeling fails to reproduce the highly potassic signature of the melt and its low H2O content. The combination of petrology, melt inclusion study, and thermodynamic modeling supports the interpretation that melt was produced by anatexis of the ultramafic boudins near peak P-T conditions, and that type 1 inclusions contain the anatectic melt that was present during garnet growth. The felsic, ultrapotassic composition of the primary anatectic melts is compatible with low melting degrees in the presence of biotite and amphibole as reactants
Molecular flexibility of polymethylene molecules: a Raman spectroscopic study
No full textThe Raman spectrum in the CH stretching region of molecules containing long alkyl residues
shows characteristic features which provide direct information on their molecular flexibility, as
probed by the C-H stretching oscillator which vibrates on the picosecond time scale. From
their Raman spectra, librational motions of the (CH2 )n units can be studied for molecules in
the solid and liquid phases. In the latter case, segmental motions must be considered. In this
paper, the spectra of hydrocarbons in the solid, liquid and as clathrates in urea and
perhydrotriphenylene are studied in terms of their overall mobility. Using molecular
dynamical calculations we show the existence of a selective coupling between CH stretchings
and skeletal torsions, which is modulated by the collective mobility of the carbon skeleton. In
particular, we account for the frequency dependence of the antisymmetic CH stretching mode
using a model which allows for selective coupling between this high frequency mode and the
low frequency torsional oscillations about the C-C bonds in the chain
Supplementary-revised - Supplemental material for Identifying treatment responders using counterfactual modeling and potential outcomes
No full textSupplemental material, Supplementary-revised for Identifying treatment responders using counterfactual modeling and potential outcomes by Raphaël Porcher, Justine Jacot, Jay S Wunder and David J Biau in Statistical Methods in Medical Research</p
- …
