@article{OmraniMoazzenOberhaenslietal.2013,
  author    = {Omrani, Hadi and Moazzen, Mohssen and Oberh{\"a}nsli, Roland and Altenberger, Uwe and Lange, Manuela},
  title     = {The Sabzevar blueschists of the North-Central Iranian micro-continent as remnants of the Neotethys-related oceanic crust subduction},
  series = {International journal of earth sciences},
  volume    = {102},
  journal   = {International journal of earth sciences},
  number    = {5},
  publisher = {Springer},
  address   = {New York},
  issn      = {1437-3254},
  doi       = {10.1007/s00531-013-0881-9},
  pages     = {1491 -- 1512},
  year      = {2013},
  abstract  = {The Sabzevar ophiolites mark the Neotethys suture in east-north-central Iran. The Sabzevar metamorphic rocks, as part of the Cretaceous Sabzevar ophiolitic complex, consist of blueschist, amphibolite and greenschist. The Sabzevar blueschists contain sodic amphibole, epidote, phengite, calcite +/- A omphacite +/- A quartz. The epidote amphibolite is composed of sodic-calcic amphibole, epidote, albite, phengite, quartz +/- A omphacite, ilmenite and titanite. The greenschist contains chlorite, plagioclase and pyrite, as main minerals. Thermobarometry of a blueschist yields a pressure of 13-15.5 kbar at temperatures of 420-500 A degrees C. Peak metamorphic temperature/depth ratios were low (similar to 12 A degrees C/km), consistent with metamorphism in a subduction zone. The presence of epidote in the blueschist shows that the rocks were metamorphosed entirely within the epidote stability field. Amphibole schist samples experienced pressures of 5-7 kbar and temperatures between 450 and 550 A degrees C. The presence of chlorite, actinolite, biotite and titanite indicate greenschist facies metamorphism. Chlorite, albite and biotite replacing garnet or glaucophane suggests temperatures of > 300 A degrees C for greenschist facies. The formation of high-pressure metamorphic rocks is related to north-east-dipping subduction of the Neotethys oceanic crust and subsequent closure during lower Eocene between the Central Iranian Micro-continent and Eurasia (North Iran).},
  language  = {en}
}
@article{SalamatZoellerZareetal.2018,
  author    = {Salamat, Mona and Z{\"o}ller, Gert and Zare, Mehdi and Amini, Mortaza},
  title     = {The maximum expected earthquake magnitudes in different future time intervals of six seismotectonic zones of Iran and its surroundings},
  series = {Journal of seismology},
  volume    = {22},
  journal   = {Journal of seismology},
  number    = {6},
  publisher = {Springer},
  address   = {Dordrecht},
  issn      = {1383-4649},
  doi       = {10.1007/s10950-018-9780-7},
  pages     = {1485 -- 1498},
  year      = {2018},
  abstract  = {One of the crucial components in seismic hazard analysis is the estimation of the maximum earthquake magnitude and associated uncertainty. In the present study, the uncertainty related to the maximum expected magnitude mu is determined in terms of confidence intervals for an imposed level of confidence. Previous work by Salamat et al. (Pure Appl Geophys 174:763-777, 2017) shows the divergence of the confidence interval of the maximum possible magnitude m(max) for high levels of confidence in six seismotectonic zones of Iran. In this work, the maximum expected earthquake magnitude mu is calculated in a predefined finite time interval and imposed level of confidence. For this, we use a conceptual model based on a doubly truncated Gutenberg-Richter law for magnitudes with constant b-value and calculate the posterior distribution of mu for the time interval T-f in future. We assume a stationary Poisson process in time and a Gutenberg-Richter relation for magnitudes. The upper bound of the magnitude confidence interval is calculated for different time intervals of 30, 50, and 100 years and imposed levels of confidence alpha = 0.5, 0.1, 0.05, and 0.01. The posterior distribution of waiting times T-f to the next earthquake with a given magnitude equal to 6.5, 7.0, and7.5 are calculated in each zone. In order to find the influence of declustering, we use the original and declustered version of the catalog. The earthquake catalog of the territory of Iran and surroundings are subdivided into six seismotectonic zones Alborz, Azerbaijan, Central Iran, Zagros, Kopet Dagh, and Makran. We assume the maximum possible magnitude m(max) = 8.5 and calculate the upper bound of the confidence interval of mu in each zone. The results indicate that for short time intervals equal to 30 and 50 years and imposed levels of confidence 1 - alpha = 0.95 and 0.90, the probability distribution of mu is around mu = 7.16-8.23 in all seismic zones.},
  language  = {en}
}
@misc{Abdollahyan2004,
  author    = {Abdollahyan, Hamid},
  title     = {The generations gap in contemporary Iran},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-47167},
  year      = {2004},
  abstract  = {This paper offers a new theoretical framework for studying the problem of generations and social change in contemporary Iran. It offers a model which is called „articulation of cultural modes". The paper agrees with Ronald Inglehart that 'culture' is now playing a more dominant role in the social formation of current societies, as 'technology' once did in the modern era. But it goes one step further by arguing that culture cannot be approached as a holistic concept building on a comprehensive theoretical framework.},
  language  = {en}
}
@misc{DonnerRoesslerKruegeretal.2011,
  author    = {Donner, Stefanie and R{\"o}ßler, Dirk and Kr{\"u}ger, Frank and Ghods, Abdolreza and Strecker, Manfred},
  title     = {Source mechanisms of the 2004 Baladeh (Iran) earthquake sequence from Iranian broadband and short-period data and seismotectonic implications},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-53982},
  year      = {2011},
  abstract  = {The northward movement and collision of the Arabian plate with Eurasia generates compressive stresses and resulting shortening in Iran. Within the Alborz Mountains, North Iran, a complex and not well understood system of strike-slip and thrust faults accomodates a fundamental part of the NNE-SSW oriented shortening. On 28th of May 2004 the Mw 6.3 Baladeh earthquake hit the north-central Alborz Mountains. It is one of the rare and large events in this region in modern time and thus a seldom chance to study earthquake mechanisms and the local ongoing deformation processes. It also demonstrated the high vulnerability of this densily populated region.},
  language  = {en}
}
@article{DonnerRoesslerKruegeretal.2013,
  author    = {Donner, Stefanie and R{\"o}ßler, Dirk and Kr{\"u}ger, Frank and Ghods, Abdolreza and Strecker, Manfred},
  title     = {Segmented seismicity of the M (w) 6.2 Baladeh earthquake sequence (Alborz Mountains, Iran) revealed from regional moment tensors},
  series = {Journal of seismology},
  volume    = {17},
  journal   = {Journal of seismology},
  number    = {3},
  publisher = {Springer},
  address   = {Dordrecht},
  issn      = {1383-4649},
  doi       = {10.1007/s10950-013-9362-7},
  pages     = {925 -- 959},
  year      = {2013},
  abstract  = {The M (w) 6.2 Baladeh earthquake occurred on 28 May 2004 in the Alborz Mountains, northern Iran. This earthquake was the first strong shock in this intracontinental orogen for which digital regional broadband data are available. The Baladeh event provides a rare opportunity to study fault geometry and ongoing deformation processes using modern seismological methods. A joint inversion for hypocentres and a velocity model plus a surface-wave group dispersion curve analysis were used to obtain an adapted velocity model, customised for mid- and long-period waveform modelling. Based on the new velocity model, regional waveform data of the mainshock and larger aftershocks (M (w) a parts per thousand yen3.3) were inverted for moment tensors. For the Baladeh mainshock, this included inversion for kinematic parameters. All analysed earthquakes show dominant thrust mechanisms at depths between 14 and 26 km, with NW-SE striking fault planes. The mainshock ruptured a 28A degrees south-dipping area of 24 x 21 km along a north-easterly direction. The rupture plane of the mainshock does not coincide with the aftershock distribution, neither in map view nor with respect to depth. The considered aftershocks form two main clusters. The eastern cluster is associated with the mainshock. The western cluster does not appear to be connected with the rupture plane of the mainshock but, instead, indicates a second activated fault plane dipping at 85A degrees towards the north.},
  language  = {en}
}
@book{NaderiReissner2012,
  author    = {Naderi, Ahmad and Reissner, Johannes},
  title     = {Schiitische Geopolitik? : zur Politik Irans im Nahen und Mittleren Osten},
  series = {WeltTrends Spezial},
  journal   = {WeltTrends Spezial},
  number    = {7},
  publisher = {Welt Trends e.V},
  address   = {Potsdam},
  isbn      = {978-3-941880-40-5},
  issn      = {2193-0627},
  pages     = {22},
  year      = {2012},
  abstract  = {Aufgrund seines umstrittenen Atomprogramms ist der Iran ein Dauerbrenner in den Medien. Doch nicht nur deshalb sollte das Land Beachtung finden. Ahmad Naderi gew{\"a}hrt uns einen Blick auf die Geopolitik des Iran, der besonders f{\"u}r die in vielen arabischen Staaten unterdr{\"u}ckten Schiiten Orientierungspunkt sein will. Doch strebt das Land die Hegemonie in der Region an? Johannes Reissner (1949-2009) analysiert das Selbstverst{\"a}ndnis des Iran und seine Verhaltensmuster. Sollte der Westen seine Politik {\"u}berdenken?},
  language  = {de}
}
@article{SalamatZoellerAmini2019,
  author    = {Salamat, Mona and Z{\"o}ller, Gert and Amini, Morteza},
  title     = {Prediction of the Maximum Expected Earthquake Magnitude in Iran:},
  series = {Pure and applied geophysics},
  volume    = {176},
  journal   = {Pure and applied geophysics},
  number    = {8},
  publisher = {Springer},
  address   = {Basel},
  issn      = {0033-4553},
  doi       = {10.1007/s00024-019-02141-3},
  pages     = {3425 -- 3438},
  year      = {2019},
  abstract  = {This paper concerns the problem of predicting the maximum expected earthquake magnitude μ in a future time interval Tf given a catalog covering a time period T in the past. Different studies show the divergence of the confidence interval of the maximum possible earthquake magnitude m_{ max } for high levels of confidence (Salamat et al. 2017). Therefore, m_{ max } should be better replaced by μ (Holschneider et al. 2011). In a previous study (Salamat et al. 2018), μ is estimated for an instrumental earthquake catalog of Iran from 1900 onwards with a constant level of completeness ( {m0 = 5.5} ). In the current study, the Bayesian methodology developed by Z{\"o}ller et al. (2014, 2015) is applied for the purpose of predicting μ based on the catalog consisting of both historical and instrumental parts. The catalog is first subdivided into six subcatalogs corresponding to six seismotectonic zones, and each of those zone catalogs is subsequently subdivided according to changes in completeness level and magnitude uncertainty. For this, broad and small error distributions are considered for historical and instrumental earthquakes, respectively. We assume that earthquakes follow a Poisson process in time and Gutenberg-Richter law in the magnitude domain with a priori unknown a and b values which are first estimated by Bayes' theorem and subsequently used to estimate μ. Imposing different values of m_{ max } for different seismotectonic zones namely Alborz, Azerbaijan, Central Iran, Zagros, Kopet Dagh and Makran, the results show considerable probabilities for the occurrence of earthquakes with Mw ≥ 7.5 in short Tf , whereas for long Tf, μ is almost equal to m_{ max }},
  language  = {en}
}
@article{SakiMoazzenOberhaensli2011,
  author    = {Saki, A. and Moazzen, Mohssen and Oberh{\"a}nsli, Roland},
  title     = {P-T evolution of the precambrian metamorphic complex, NW Iran a study of metapelitic rocks},
  series = {Geological journal},
  volume    = {46},
  journal   = {Geological journal},
  number    = {1},
  publisher = {Wiley-Blackwell},
  address   = {Malden},
  issn      = {0072-1050},
  doi       = {10.1002/gj.1236},
  pages     = {10 -- 25},
  year      = {2011},
  abstract  = {The Mahneshan Metamorphic Complex (MMC) is one of the Precambrian terrains exposed in the northwest of Iran. The MMC underwent two main phases of deformation (D-1 and D-2) and at least two metamorphic events (M-1 and M-2). Critical metamorphic mineral assemblages in the metapelitic rocks testify to regional metamorphism under amphibolite-facies conditions. The dominant metamorphic mineral assemblage in metapelitic rocks (M-1) is muscovite, biotite I, Garnet I, staurolite, Andalusite I and sillimanite. Peak metamorphism took place at 600-620 degrees C and similar to 7 kbar, corresponding to a depth of ca. 24 km. This was followed by decompression during exhumation of the crustal rocks up to the surface. The decrease of temperature and pressure during exhumation produced retrograde metamorphic assemblages (M-2). Secondary phases such as garnet II biotite It. Andalusite II constrain the temperature and pressure of M, retrograde metamorphism to 520-560 degrees C and 2.5-3.5 kbar, respectively. The geothermal gradient obtained for the peak of metamorphism is 33 degrees C km(-1), which indicates that peak metamorphism was of Barrovian type and occurred under medium-pressure conditions. The MMC followed a 'clockwise' P T path during metamorphism, consistent with thermal relaxation following tectonic thickening. The bulk chemistry of the MMC metapelites shows that their protoliths were deposited at an active continental margin. Together with the presence of palaeo-suture zones and ophiolitic rocks around the high-grade metamorphic rocks of the MMC, these features suggest that the Iranian Precambrian basement formed by an island-arc type cratonization.},
  language  = {en}
}
@book{OPUS4-4486,
  title     = {Naher Osten : Politik und Gesellschaft},
  editor    = {Schmidt, Renate},
  publisher = {Berliner Debatte Wissenschaftsverlag},
  address   = {Berlin},
  isbn      = {978-3-931703-29-5},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-46806},
  publisher      = {Universit{\"a}t Potsdam},
  year      = {1998},
  abstract  = {Der dritte Band der Potsdamer Textb{\"u}cher befasst sich mit gesellschaftlichen Entwicklungen im konfliktreichen Nahen Osten. Die Zusammenstellung der Texte erfolgte sowohl mit Blick auf die anhaltende Kulturkreisdiskussion als auch hinsichtlich der Bem{\"u}hungen um Stabilit{\"a}t in dieser Region. Hinzu kommen Analysen zur wirtschaftlichen Entwicklung und den politischen Regimes in Israel, Pal{\"a}stina, {\"A}gypten, im Jemen und Iran. Ausz{\"u}ge aus Verfassungen arabischer Staaten, statistische Angaben und eine Bibliographie vervollst{\"a}ndigen das Textbuch.},
  language  = {de}
}
@misc{Zamirirad2013,
  author    = {Zamirirad, Azadeh},
  title     = {Mit dem Schl{\"u}ssel zum Erfolg : Irans neuer Pr{\"a}sident ; ein Kommentar},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-67881},
  year      = {2013},
  abstract  = {Iranische Pr{\"a}sidentschaftswahlen sind immer f{\"u}r eine {\"U}berraschung gut. Noch eine Woche vor der Wahl d{\"u}rften die wenigsten mit einem Erdrutschsieg Hassan Rouhanis gerechnet haben. Der neue Mann ist dabei ein Altbekannter. Zahlreiche Posten hat er in der Islamischen Republik bereits bekleidet und sich als Chefunterh{\"a}ndler auch im Ausland einen Namen gemacht. Welche Erwartungen werden an ihn gerichtet und welche Herausforderungen gilt es nun zu meistern?},
  language  = {de}
}