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Antisemitism in muslim communities and muslim countries: debates and studies of a complex issue
(2015)
In this article, I discuss surveys, academic debates, and research on antisemitism among Muslims in Muslim-majority countries and in Europe today. After a review of antisemitism in both cases, different explanations for its causes are presented. Negative attitudes towards Jews in Muslim countries are the rule, not the exception. An important factor in almost all Muslim countries are anti-Zionist attitudes and agitations that are mixed with antisemitic stereotypes and conspiracy theories. In Europe, antisemitism is more prevalent among Muslims than among non-Muslims and Muslims are disproportionately often involved in antisemitic incidents.
It turns out that antisemitism among Muslims is manifested in many ways and that it has many causes. One-dimensional explanations are not sufficient. Arguments that antisemitism is primarily a result of the Middle East conflict or of discrimination/colonization seem to be outdated in view of new research. Historically, the interaction of Arab nationalism, Islamist movements, and the collaboration with the Nazis in the middle of the 20th century played a significant role in ensuring that the discriminatory treatment of Jews in Islam in the Middle Ages did not disappear in the course of establishing nation states, but was converted to a large extent into antisemitism. Today, Islamist influences and stereotypes that are passed on by media and within social circles are essential factors for the prevalence of antisemitic attitudes among Muslims.
Beyond the line?
(2004)
In December 2003, the Orient-Occident Forum for Intercultural Exchange at the University of Potsdam and the academic partnership program Potsdam-Teheran held a week-long conference, titled „Comparing Processes of Modernization“, which was attended by many social scientists from Egypt, Iran and Germany. In this issue, some of the contributions of the conference are published and commented. During the course of the conference, an intercultural discourse – „beyond the line“ – concerning the responsibilities and development prospects of modernization theory took place. In their article, the organizers of the meeting try to systematically summarize these discussions and present some further reflections.
Die faulige Luft aus dem tiefsten Mittelalter, denken sich zivilisierte Mitteleuropabewohnende, und sind erstaunt zu erfahren, dass es im Iran heute legal ist, sich von einer Frau in einen Mann umoperieren zu lassen, oder umgekehrt. Noch besser: Die Geschlechtsumwandlung wird von der Krankenkasse bezahlt.
Das Ende der Theokratie?
(2010)
Iran steht vor einer neuen Revolution. Die Wahlen und deren offensichtlicher Betrug haben die Spaltung des Landes zu Tage gefördert. Die theokratische Herrschaft kann sich nur noch durch einen ölgeförderten Klientelismus am Leben erhalten und steht nun dort, wo der Schah vor dreißig Jahren gestanden hat. Nur durch eine kluge Politik, die auch Versöhnung bietet, kann ein friedlicher Machtwechsel herbeigeführt und die Demokratisierung des Landes ermöglicht werden.
Das politische System Irans
(2009)
Seit nunmehr 30 Jahren hat die Islamische Republik Iran Bestand, doch noch immer dauern Debatten über die Einordnung des politischen Systems an. Handelt es sich um ein autoritäres oder totalitäres Regime oder gar um eine neue Form islamischer Herrschaft? Die Beantwortung der Frage ist nicht nur für die Wissenschaft von Relevanz; sie ist von hoher politischer Aktualität. In zehn Beiträgen von deutschen und iranischen Autoren wird das politische System der Islamischen Republik anhand seiner Geschichte, seines Institutionengefüges, seiner gesellschaftlichen Kräfte sowie seiner Außenbeziehungen analysiert und in das regionale Gefüge eingeordnet. Ergänzt werden die Artikel durch Schaubilder und Statistiken sowie durch eine Zeittafel und ein Glossar mit den wichtigsten Begrifflichkeiten.
There have been three main phases of political discourse in recent Iranian history. A paternalistic era was accompanied by a phase of absolutistic rule during the Qagar dynasty. This phase was followed by a forced modernization, when the Shah of Iran expanded his absolutistic rule and established a dictatorship. With the Islamic Revolution of 1979, a new phase of political discourse emerged with a tendency towards religious traditionalism. The author states that religion and democracy are not in opposition. However, there is need for dialogue between the East and the West.
Die vorliegende Schrift "Die Islamische Republik Iran" erwächst aus der Durchführung sowie der Vor- und Nachbereitung einer Studienreise von Studenten in den Iran. Im Herbst 2004 reist die Gruppe nach Teheran und lernt neben den dem Alborz-Gebirge und der Kaspi-Region auch die Städte Shiraz, Persepolis, Yazd und Esfahan kennen. In acht Einzelbeiträgen vermitteln die Studenten unter dem Eindruck des selbst Gesehenen und Erlebten und in der Literatur Erarbeiteten einen Überblick zum politisch-administrativen System der Islamischen Republik Iran, zur Wirtschaft, zur Bevölkerungsentwicklung, zur Stadtstruktur im islamischen Orient und in der Hauptstadt, zur Migration im Zusammenhang mit dem Iran-Irak-Krieg, zur Binnenwanderung sowie zu ausgewählten Aspekten der Außenpolitik.
Sanktionen sind ein wichtiges Instrument des UN-Sicherheitsrats zur Erhaltung des Weltfriedens. Viele zentrale Entscheidungen, wie etwa die Listung und Entlistung terrorverdächtiger Personen, werden fernab der Öffentlichkeit in Sanktionsausschüssen getroffen. Die Einsetzung dieser Ausschüsse hat die Entscheidungsdynamiken im Rat erheblich verändert.
The tectonically driven growth of mountains reflects the characteristics of the underlying fault systems and the applied tectonic forces. Over time, fault networks might be relatively static, but stress conditions could change and result in variations in fault slip orientation. Such a tectonic landscape would transition from a simple to a composite state: the topography of simple landscapes is correlated with a single set of tectonic boundary conditions, while composite landscapes contain inherited topography due to earlier deformation under different boundary conditions. We use fault interaction modeling to compare vertical displacement fields with topographic metrics to differentiate the two types of landscapes. By successively rotating the axis of maximum horizontal stress, we produce a suite of vertical displacement fields for comparison with real landscapes. We apply this model to a transpressional duplex in the south central Alborz Mountains of Iran, where NW oriented compression was superseded by neotectonic NE compression. The consistency between the modeled displacement field and real landforms indicates that the duplex topography is mostly compatible with the modern boundary conditions, but might include a small remnant from the earlier deformation phase. Our approach is applicable for various tectonic settings and represents an approach to identify the changing boundary conditions that produce composite landscapes. It may be particularly useful for identifying changes that occurred in regions where river profiles may no longer record a signal of the change or where the spatial pattern of uplift is complex.
The complex system of strike-slip and thrust faults in the Alborz Mountains, Northern Iran, are not well understood yet. Mainly structural and geomorphic data are available so far. As a more extensive base for seismotectonic studies and seismic hazard analysis we plan to do a comprehensive seismic moment tensor study also from smaller magnitudes (M < 4.5) by developing a new algorithm. Here, we present first preliminary results.
Erweiterte Momententensorinversion und ihre seismotektonische Anwendung : Elbursgebirge, Nordiran
(2009)
Der Elburs im Norden Irans ist ein durch die Konvergenz der Arabischen und Eurasischen Platte verursachtes doppelt konvergentes Gebirge. Das komplexe System von Blattverschiebungen und Überschiebungen sowie die Aufnahme der Deformation im Elburs ist noch nicht sehr gut verstanden. Eine neu zu entwicklende Methode zur Inversion von seismischen Momententensoren, die unterschiedliche Beobachtungen verschiedener Stationstypen kombiniert invertiert, soll die bisher hauptsächlich strukturelle/geomorphologische Datengrundlage um Momententensoren auch kleinerer Magnituden (M < 4.5) erweitern. Dies ist die notwendige Grundlage für detaillierte seismotektonische Studien, die wiederum die Basis für seismische Gefährdungsanalysen bilden.
The seismically active Alborz mountains of northern Iran are an integral part of the Arabia-Eurasia collision. Linked strike-slip and thrust/reverse-fault systems in this mountain belt are characterized by slow loading rates, and large earthquakes are highly disparate in space and time. Similar to other intracontinental deformation zones such a pattern of tectonic activity is still insufficiently understood, because recurrence intervals between seismic events may be on the order of thousands of years, and are thus beyond the resolution of short term measurements based on GPS or instrumentally recorded seismicity. This study bridges the gap of deformation processes on different time scales. In particular, my investigation focuses on deformation on the Quaternary time scale, beyond present-day deformation rates, and it uses present-day and paleotectonic characteristics to model fault behavior. The study includes data based on structural and geomorphic mapping, faultkinematic analysis, DEM-based morphometry, and numerical fault-interaction modeling. In order to better understand the long- to short term behavior of such complex fault systems, I used geomorphic surfaces as strain markers and dated fluvial and alluvial surfaces using terrestrial cosmogenic nuclides (TCN, 10Be, 26Al, 36Cl) and optically stimulated luminescence (OSL). My investigation focuses on the seismically active Mosha-Fasham fault (MFF) and the seismically virtually inactive North Tehran Thrust (NTT), adjacent to the Tehran metropolitan area. Fault-kinematic data reveal an early mechanical linkage of the NTT and MFF during an earlier dextral transpressional stage, when the shortening direction was oriented northwest. This regime was superseded by Pliocene to Recent NE-oriented shortening, which caused thrusting and sinistral strike-slip faulting. In the course of this kinematic changeover, the NTT and MFF were reactivated and incorporated into a nascent transpressional duplex, which has significantly affected landscape evolution in this part of the range. Two of three distinctive features which characterize topography and relief in the study area can be directly related to their location inside the duplex array and are thus linked to interaction between eastern MFF and NTT, and between western MFF and Taleghan fault, respectively. To account for inferred inherited topography from the previous dextral-transpression regime, a new concept of tectonic landscape characterization has been used. Accordingly, I define simple landscapes as those environments, which have developed during the influence of a sustained tectonic regime. In contrast, composite landscapes contain topographic elements inherited from previous tectonic conditions that are inconsistent with the regional present-day stress field and kinematic style. Using numerical fault-interaction modeling with different tectonic boundary conditions, I calculated synoptic snapshots of artificial topography to compare it with the real topographic metrics. However, in the Alborz mountains, E-W faults are favorably oriented to accommodate the entire range of NW- to NE-directed compression. These faults show the highest total displacement which might indicate sustained faulting under changing boundary conditions. In contrast to the fault system within and at the flanks of the Alborz mountains, Quaternary deformation in the adjacent Tehran plain is characterized by oblique motion and thrust and strike-slip fault systems. In this morphotectonic province fault-propagation folding along major faults, limited strike-slip motion, and en-échelon arrays of second-order upper plate thrusts are typical. While the Tehran plain is characterized by young deformation phenomena, the majority of faulting took place in the early stages of the Quaternary and during late Pliocene time. TCN-dating, which was performed for the first time on geomorphic surfaces in the Tehran plain, revealed that the oldest two phases of alluviation (units A and B) must be older than late Pleistocene. While urban development in Tehran increasingly covers and obliterates the active fault traces, the present-day kinematic style, the vestiges of formerly undeformed Quaternary landforms, and paleo earthquake indicators from the last millennia attest to the threat that these faults and their related structures pose for the megacity.
The Northern Central Iranian Micro-continent (CIM) represents Neotethys-related oceanic crust remnants, emplaced due to convergence between CIM and Eurasia plates during Eocene. Mafic and ultramafic units are exposed along the northern part of the CIM in the Sabzevar area. The geology and field relation of Sabzevar ophiolite indicate northward subduction of the Sabzevar basin. The average whole rock chemistry of mafic (gabbros) and ultramafic samples (lherzolite, harzburgite and dunite) is characterized by a range of MgO of 11.16-31.88, CaO 5.22-11.53 and Al2O3 2.77-14.57, respectively. Low LREE/HREE ratio of ultramafic samples is accompanied by enrichment of large ion lithophile elements (LILE) such as Sr, Pb and K. Mafic samples show two distinct groups with low and high LREE/HREE ratios. The spider diagram of mafic samples indicates enrichment in Sr, Pb and K and depletion in REE. Petrological and geochemical evidence and field relations show that the mafic rocks formed in a supra-subduction zone setting. Petrological studies reveal the role of fractional crystallization and assimilation effect by released fluids during subduction related generation of the Sabzevar mafic rocks. We suggest that the studied mafic rocks likely represent the basement of an initial island arc, which was generated in a supra-subduction zone setting within the Neotethys branch of the Sabzevar Ocean at the north of CIM. Copper, gold and chromite mineralizations are studied in relation to island arc setting and supra-subduction environment. Similarities in lithology, ophiolite age and mineralization between Sabzevar ophiolite and Bardaskan-Torbat Heydariyeh ophiolites testify for their separation due to rotation (or faulting) of the Central Iranian Micro-continent.
Im Zentrum steht die Genese einer sich im 20. Jahrhundert zunehmend ideologisierenden Schia, deren wachsende diskursive Macht sich mit der Iranischen Revolution von 1979 durch die Schaffung realpolitischer Strukturen in Form der velayāt-e faqih niederzuschlagen vermag. Untersucht wird, unter welchen Bedingungen der gesellschaftspolitische Entwurf des schiitischen Klerus sich auch im Hinblick auf existierende nicht-religiöse Gegendiskurse seiner Zeit – etwa aus der staatlichen Bürokratie, Intellektuellenzirkeln oder aus linken und nationalen Bewegungen – wandelte. Wie begegnete der Klerus den drängenden gesellschaftlichen Fragen der Moderne und wie wird der politische Diskurs heute geführt?
Irans zunehmender Einfluss als Regionalmacht wird wegen seines Atomprogramms und seiner antiwestlichen Politik als Störfaktor bewertet. Die offensive Rhetorik Teherans zielt primär darauf ab, möglichen Gefahren entgegenzutreten. Westliche Politik sollte das allseitig bestehende Interesse an regionaler Stabilität nutzen, um seine ausschließlich auf Eindämmung bedachte Politik zu überwinden.
Das Paper untersucht die geopolitische Konfrontation zwischen Iran und den USA sowie deren Auswirkung auf eine Veränderung der bestehenden Weltordnung. Es wird deutlich, dass die US-amerikanische Sanktionspolitik nicht nur auf das Nuklearprogramm abzielt, sondern grundsätzlich versucht, die Wirtschaftskraft der unabhängig von den Interessen der USA agierenden Regionalmacht zu brechen. Doch die Sanktionspolitik konnte weder eine Lösung des Nukleardossiers herbeiführen noch die Wirtschaftskraft Irans eindämmen. Es ist Zeit für eine fundamentale Kursänderung.
Die Frage nach einer veränderten Strategie des Westens im Atomkonflikt mit dem Iran ist wieder virulent. Bereits auf seiner ersten Pressekonferenz hat der als gemäßigt geltende neue iranische Präsident Hassan Ruhani mehr Transparenz über das Atomprogramm seines Landes in Aussicht gestellt. Ob sich damit ein Fenster der Möglichkeiten öffnet, den Konflikt doch noch einvernehmlich und vor allem friedlich zu lösen, muss sich erweisen.
Die zehnten Präsidentschaftswahlen im Iran sorgten für einen Eklat. Ausgerechnet im Jubiläumsjahr, in dem man sich mit Stolz präsentieren wollte, erlebt die Islamische Republik ihren größten Legitimitätsverlust. Mit der Verkündung von Ahmadinedschads Wahlsieg löste das Regime eine Welle der Empörung aus, die bis heute nicht abgeklungen ist. Zwar konnten die Proteste den amtierenden Präsidenten nicht von seiner zweiten Amtszeit abhalten, doch der grüne Sommer hat seine Spuren in der Theokratie hinterlassen.
The Makran accretionary prism in SE Iran and SW Pakistan is one of the most extensive subduction accretions on Earth. It is characterized by intense folding, thrust faulting and dislocation of the Cenozoic units that consist of sedimentary, igneous and metamorphic rocks. Rock units forming the northern Makran ophiolites are amalgamated as a melange. Metamorphic rocks, including greenschist, amphibolite and blueschist, resulted from metamorphism of mafic rocks and serpentinites. In spite of the geodynamic significance of blueschist in this area, it has been rarely studied. Peak metamorphic phases of the northern Makran mafic blueschist in the Iranshahr area are glaucophane, phengite, quartz +/- omphacite+epidote. Post peak minerals are chlorite, albite and calcic amphibole. Blueschist facies metasedimentary rocks contain garnet, phengite, albite and epidote in the matrix and as inclusions in glaucophane. The calculated P-T pseudosection for a representative metabasic glaucophane schist yields peak pressure and temperature of 11.5-15kbar at 400-510 degrees C. These rocks experienced retrograde metamorphism from blueschist to greenschist facies (350-450 degrees C and 7-8kbar) during exhumation. A back arc basin was formed due to northward subduction of Neotethys under Eurasia (Lut block). Exhumation of the high-pressure metamorphic rocks in northern Makran occurred contemporarily with subduction. Several reverse faults played an important role in exhumation of the ophiolitic and HP-LT rocks. The presence of serpentinite shows the possible role of a serpentinite diapir for exhumation of the blueschist. A tectonic model is proposed here for metamorphism and exhumation of oceanic crust and accretionary sedimentary rocks of the Makran area. Vast accretion of subducted materials caused southward migration of the shore.
For the first time when the new Islamic councils began their Operation, many intellectuals and politicians proclaimed that there would be no room for the young Islamic councils to proceed. In political terms, because of the new challenges between the rightists and leftists, many people had no hope to see the results of the councils. Still others believed that under the dominating ruling system of Iran there is no space for public opinion and participation in local decision-making. This paper focuses on the role of the Islamic Councils as a new form of social democracy, which decentralizes power and creates good local governance. The paper also discusses the obstacles for the Councils in the development of the region.