2,362 research outputs found
Matthias Wagner : author profile
No full textThe author presented on this page has published his 10. article in Angewandte Chemie in the last 10 years
Déformation intraplaque de la lithosphère océanique indo-australienne: cinématique, réactivation et serpentinisation
No full textLa déformation intraplaque équatoriale dans l’océan Indien, séparant l’Inde et l’Australie,intrigue depuis plusieurs décennies de par sa nature diffuse qui tranche avec la notionclassique de plaque rigide dont les frontières sont localisées. C’est également un évènementimportant de la géodynamique de l’Asie puisqu’on peut considérer cette déformation commeun contre coup de la collision himalayenne.Nous dérivons pour la première fois le champ de déformation intraplaque instantanée contraintà la fois par le GPS en champ lointain et par le style des séismes intraplaques. La cinématiquepermet de montrer le rôle moteur de l’Australie dans le déclenchement de la déformation intraplaquepar son accélération vers le nord. L’âge de l’initiation de la déformation actuelle apu être redéfini à partir de profils sismiques. Ceux ci enregistrent la déformation dans les sédimentsdu Bengale depuis 9Ma. La cinématique instantanée est en excellent accord avec uncontinuumde déformation de 9Ma à l’actuel.Le champde déformation instantané requiert un Bassin central indien rhéologiquement faiblepour satisfaire le style de déformation observé. On rapproche ce résultat de l’anomalie de fluxde chaleur détectée dans la zone de déformation et très corrélée spatialement aux failles. Desdifférentes sources de chaleur envisagées, nous montrons grâce à des modèles thermiquesque seul l’effet de la serpentinisation exothermique du manteau permet d’expliquer l’anomalieobservée. Celle-ci n’est donc pas une cause de la déformation mais une conséquencepuisque ce sont les failles qui hydratent le manteau. La serpentinisation produit donc unechute brutale du coefficient de friction des failles du Bassin central indien et une anomaliethermique transitoire.Le réseau de failles inverses du Bassin central indien est un excellent laboratoire àgrande échelle pourmieux comprendre les processus d’initiation et de localisation d’une déformationnaissante. Nos nouvelles données sismiques indiquent une réactivation massivede la fabrique océanique sous l’effet d’une compression convenablement orientée. La déformationactuelle n’est cependant localisée que sur une sélection de failles réactivées et nousmontrons à l’aide d’un modèle aux éléments finis qu’un abandon de failles peut effectivementse produire en passant d’un adoucissement rhéologique sensible à la déformation lorsde la phase de réactivation à un adoucissement au taux de déformation lorsque les failles sontmatures.La même fabrique océanique a été réactivée de façon spectaculaire suite au mégaséisme deBanda Aceh (Mw=9.3) immédiatement suivi par le séisme de Nias (Mw=8.7). On peut doncétudier son comportement à beaucoup plus courte échelle de temps sous l’effet des variationsde contraintes co-sismiques. Cette sismicité induite est préférentiellement décrochanteet correspond à une réactivation à court terme des zones de fractures du Bassin de Wharton.C’est donc le même style de déformation qui est prépondérant à court et à long terme, sousl’effet de la traction de la lithosphère océanique du Bassin de Wharton au fossé de Sumatra.Plate tectonics usually describes rigid plates limited by narrow boundaries. It is howevernot always true and diffuse boundaries are quite frequent (Figure 1), particularly on thecontinents. Among the known diffuse deformation zones, the central Indian ocean clearly appearsas a singularity because of its exceptional size and because deformation occurs in theoceanic lithosphere (Figure 1). Furhter, the thick sedimentation from the Bengal fan allowsthe unravelling of the history of deformation since the lateMiocene through seismic profiles.Intraplate diffuse deformation between India and Australia is thus the ideal place to study thelocalization processes of a nascent deformation and the role of preexistant structures, sincethe structural heritage is much more simple in the oceanic domain.In a first chapter,we present the formation of the Indian Ocean starting with the GondwanaBreakup.We focus on the India-Asutralia plate and discuss the different steps leading tothe formation of the Central Indian Basin (CIB), the NinetyEast Ridge (NyR) and the WhartonBasin (WB). We then discuss the concept of diffuse boundary between India and Australia,detailing the different styles of deformation from seismicity and new seismic profiles.In a second chapter, we will focus on the age of the onset of deformation using seismic profilesand ODP holes. The evolution of deformation is also discussed in a paper published inGeophysical Journal International (Delescluse et Chamot-Rooke, 2007). This paper presentsthe instantaneous deformation field and the associated velocity field derived from GPS andfocal mechanisms. The instantaneous kinematics is in good agreement with a continuum ofdeformation since lateMiocene.The next chapter deals with the localization processes in the CIB. First, we study the origin ofthe heat-flow anomaly which seems correlated to reverse faults. Heat-flow is used as a proxyfor the rheology of the lithosphere in our best kinematic model but its origin remains unknown.In a paper published in Earth and Planetary Science Letters (Delescluse et Chamot-Rooke, 2008), we propose that the thermal anomaly is a result of the exothermic serpentinizationof the oceanic mantle. We show that the thermal anomaly is a consequence of deformationand is not preexistant. The equatorial localization of deformation is best explained bythe reactivation of paleo-normal faults from the oceanic fabric when large intraplate stressesare correctly oriented. Using high resolution seismic profiles and a finite element model, weshow in a paper published in Geophysical Research Letters (Delescluse et al., 2008) that followingfull reactivation, faults are selectively abandoned because of the weakening of some ofthe fault planes.In a last chapter, we show that the Aceh (2004) and Nias (2005) megathrust earthquakes actedas an intraplate seismicity "accelerator" in the near-trench oceanic plate (Wharton Basin).Using Coulomb stress variations, we show that these subduction earthquakes favor theoccurence of left-lateral strike-slip along N-S paleo-transform faults rather than neoformedNE-SWreverse faults
Enduring Ambiguity: What Is European Literature? Matthias Nawrat in Conversation with Monika Woltig
No full textMatthias Nawrat is a Polish-German author living in Germany born in Opole, Poland. He moved with his family to Bamberg in 1989. He was awarded the Adelbert-von-ChamissoFörderpreis, was nominated for the Deutscher Buchpreis, received the Bremen Literature Prize and the Alfred Döblin Medaille. His most important novels were "Wir zwei allein" (2012), "Die vielen Tode unseres Opas Jurek" (2015), and "Der traurige Gast" (2019).Matthias Nawrat to niemiecki autor polskiego pochodzenia. Matthias Nawrat urodził się w Opolu i wraz z rodziną przeprowadził się w 1989 roku do Bambergu. Uzyskał Nagrodę im. Adelberta von Chamisso (Förderpreis), był nominowany do Niemieckiej Nagrody Książkowej (Deutscher Buchpreis), otrzymał Nagrodę Literacką miasta Bremy i Medal im. Alfreda Döblina. Najważniejsze teksty: "Wir zwei allein" (2012), "Die vielen Tode unseres Opas Jurek" (2015), "Der traurige Gast" (2019).Matthias Nawrat ist ein deutscher Autor polnischer Herkunft. Matthias Nawrat wurde im polnischen Opole geboren und siedelte 1989 mit seiner Familie nach Bamberg über. Er wurde mit dem Adelbert-von-Chamisso-Förderpreis ausgezeichnet, zum Deutschen Buchpreis nominiert und erhielt den Bremer Literaturpreis sowie die Alfred-Döblin-Medaille. Die wichtigsten Texte: "Wir zwei allein" (2012), "Die vielen Tode unseres Opas Jurek" (2015), "Der traurige Gast" (2019)
Baculus Militaris Compendiosus Infanterie Oder Officirers Stab Das ist Ein kurtzer Begrieff der Kriegs Lectionen bey dem Fußvolck gebräuchlich auch nötig : Bestehend in sechserley Exercitien 1. In der Partisan, halber Pique oder Jägerstock. 2. In der Fahn. 3. In der Pique. 4. In der Musqueten. 5. In der Musqueten mit der gabel oben und unten mit einer eiserner spitzen und in der mitten mit einem ein geschrobenen hacken. 6. In Hieb degen/ welcher bey dem fußvolck brauchlich / [Matthias Schlüter]
No full textJohn Matthias
No full textPoster promoting author John Matthias reading from his work in the Auditorium, Building 9, University of North Florida.
Poster dimensions: 26.7 cm x 41.8 cmhttps://digitalcommons.unf.edu/performances_print/1013/thumbnail.jp
Patristical Ideas in the Works of Matthias of Janov
No full textANGLICKÁ ANOTACE Title: Patristical ideas in the works of Matthias of Janov The thesis treats of the identification of ideas of church fathers in the work and thinking of Matthias of Janov. The thesis consits of three main parts. First part deals with Matthias of Janov in broader context of church tradition. Major political and theological developments that could have an impact on Matthias theological work are presented in this section. Second part introduces life of Matthias of Janov and identifies his major theological contributions. In the third part of the thesis, following explanation of methodology used, the findings of the author are presented. Three areas were selected by the author and researched in view of the identification of possible influance of church fathers in the Matthias of Janov work: the idea of Antichrist, frequent eucharisty and condemnation of idolatry. The findings confirm a strong influance of Augustin and Hieronymus in particular and other early church fathers on the formation of the theology of Matthias of Janov in all three areas of the study. It was also noticed that through the church fathers Matthias of Janov was strongly influenced by neoplatonism which was documented on his idea of "The First Thruth" Key words: Matthias of Janov, church fathers, antichrist, eucharisty,..
Foreign Policy of King Matthias Corvinus from 1464 to 1490
No full textOvaj je članak drugi dio rada u kojem se istražuje vrlo kompleksna europska politika ugarsko-hrvatskoga kralja Matijaša Korvina. U ovom se dijelu razmatraju događaji od proljeća 1464. do 1490. godine. U prvom poglavlju članka autor obrađuje pokušaj organiziranja križarskoga pohoda Pija II. protiv Osmanlija 1464. i Matijaševe samostalne akcije radi učvršćivanja jugoistočnih granica kraljevstva. U drugom se poglavlju obrađuje razvoj Matijaševih odnosa s bivšim tastom Jurjem Podjebradskim koji je na kraju doveo do rata (1468–1471). U trećem je poglavlju dan kratak osvrt na pobunu plemstva protiv Matijaševe centralističke vladavine 1472. Četvrto se poglavlje bavi ratom za češko prijestolje (1471–1479) i ponovnim ratom protiv Fridrika III. (1477). U petom poglavlju autor daje kratki pregled Matijaševih odnosa s papinstvom, a u šestom pregled ratovanja s Osmanlijama tijekom sedamdesetih i osamdesetih godina XV. stoljeća. U sedmom poglavlju razmatraju se diplomatske akcije vezane uz traženje Matijaševe nove supruge te njegov brak s Beatricom Aragonskom. U osmom poglavlju autor se bavi Matijaševim ratom s Fridrikom III. za carsku titulu. Deveto je poglavlje posvećeno kraljevoj vanjskoj politici i diplomatskim aktivnostima s Venecijom i talijanskim državama tijekom osamdesetih godina. Deseto poglavlje daje pregled političkih aktivnosti tijekom posljednjih godina njegove vladavine. Jedanaesto poglavlje analizira Matijaševu vojsku. Rad završava kratkim pregledom posljednica kraljeve burne politike.This article is the second part of a longer paper in which the author reviews the very complex foreign policy of Hungarian-Croatian king Matthias Corvinus. In this paper the author analyses major events from Matthias’ coronation in the spring of 1464 until his sudden death in Vienna in the spring of 1490. The whole paper and analysis of events are based on research of various sources and literature. In the first chapter the author describes the failed attempt of Pope Pius II to organize a crusade against the Ottoman Empire in 1464 and Matthias’ own actions against the Turks with the main goal of strengthening his southeastern borders. In the second chapter the author analyses the conflict between Matthias and his ex-father-in-law, George of Poděbrady, and the war between them (1468–1471). In the third chapter the author gives a short overview of the uprising of magnates and the aristocracy against the central rule of King Matthias (1472). The fourth chapter deals with the war for the Bohemian throne from 1471 to 1479 and the war against Frederick III in 1477. In the next chapter the author gives a brief overview of the diplomatic relations between popes and Matthias Corvinus over a longer period of time, from 1464 to 1490. The main subject of the sixth chapter is the war against the Ottoman Empire during the seventh and eighth decade of the 15th century. In the seventh chapter the author describes Matthias’ search for his next wife and his marriage to Beatrice of Aragon. In the following chapter the author reviews Matthias’ new war against Frederick III for the title of the German Empire. The ninth chapter is a brief overview of Matthias’ foreign policy in the Italian states and Venice during the last decade of his life. The tenth chapter is dedicated to the final years of Matthias’ life. The next chapter analyses one of the most important segments of his foreign policy – his army. This article ends with short overview of the events which happened after the death of King Matthias and the consequences of his stormy policy
Achieving sustainable reorganization after bankruptcy: empirical evidence from formal proceedings of Austrian SMEs
No full textAuthor Matthias Baschinger, BScMasterarbeit Universität Linz 202
Achieving sustainable reorganization after bankruptcy: empirical evidence from formal proceedings of Austrian SMEs
No full textAuthor Matthias Baschinger, BScMasterarbeit Universität Linz 202
Mechanical and fire resistance properties of jute/pp composites with intumescent flame retardant
No full textAuthor Matthias Eckerstorfer, BScKurzfassungen in deutscher und englischer SpracheMasterarbeit Universität Linz 201
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