Littérature scientifique sur le sujet « Makran (Iran) »
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Articles de revues sur le sujet "Makran (Iran)"
Hafeez Abbasi, Muhammad Imran. « IS MAKRAN A SEPARATE MICROPLATE ? A SHORT REVIEW ». MALAYSIAN JOURNAL OF GEOSCIENCES 5, no 1 (19 novembre 2020) : 01–05. http://dx.doi.org/10.26480/mjg.01.2021.01.05.
Texte intégralDelavar, M. R., H. Mohammadi, M. A. Sharifi et M. D. Pirooz. « TSUNAMI RISK ASSESSMENT MODELLING IN CHABAHAR PORT, IRAN ». ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLII-2/W7 (12 septembre 2017) : 461–67. http://dx.doi.org/10.5194/isprs-archives-xlii-2-w7-461-2017.
Texte intégralKhan, Waseem, et Mahnoor Mirwani. « PROBING THE NATURE AND CHARACTERISTICS OF ACTIVE MUD VOLCANIC CLUSTERS IN MAKRAN COASTAL ZONE, PAKISTAN ». International Journal of Research -GRANTHAALAYAH 8, no 3 (25 mai 2020) : 214–22. http://dx.doi.org/10.29121/granthaalayah.v8.i3.2020.145.
Texte intégralNormand, Raphaël, Guy Simpson, Frédéric Herman, Rabiul Haque Biswas et Abbas Bahroudi. « Holocene Sedimentary Record and Coastal Evolution in the Makran Subduction Zone (Iran) ». Quaternary 2, no 2 (12 juin 2019) : 21. http://dx.doi.org/10.3390/quat2020021.
Texte intégralSafari, A., A. M. Abolghasem, N. Abedini et Z. Mousavi. « ASSESSMENT OF OPTIMUM VALUE FOR DIP ANGLE AND LOCKING RATE PARAMETERS IN MAKRAN SUBDUCTION ZONE ». ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLII-4/W4 (27 septembre 2017) : 523–29. http://dx.doi.org/10.5194/isprs-archives-xlii-4-w4-523-2017.
Texte intégralAyub, Mubarak, et Safi Ullah Khan Marwat. « State and Society under the Zikris in Makran : A Historical Account ». Global Social Sciences Review VIII, no II (30 juin 2023) : 108–18. http://dx.doi.org/10.31703/gssr.2023(viii-ii).11.
Texte intégralHaberland, Christian, Mohammad Mokhtari, Hassan Ali Babaei, Trond Ryberg, Mehdi Masoodi, Abdolreza Partabian et Jörn Lauterjung. « Anatomy of a crustal-scale accretionary complex : Insights from deep seismic sounding of the onshore western Makran subduction zone, Iran ». Geology 49, no 1 (13 août 2020) : 3–7. http://dx.doi.org/10.1130/g47700.1.
Texte intégralNormand, Raphaël, Guy Simpson et Abbas Bahroudi. « Extension at the coast of the Makran subduction zone (Iran) ». Terra Nova 31, no 6 (30 juillet 2019) : 503–10. http://dx.doi.org/10.1111/ter.12419.
Texte intégralNegaresh, Hossein. « Mud volcanoes in Sistan and Baluchestan Provinces, Makran Coast, Southeast Iran ». Bulletin of the Geological Society of Malaysia 54 (1 novembre 2008) : 1–7. http://dx.doi.org/10.7186/bgsm54200801.
Texte intégralNemati, Majid. « Seismotectonic and seismicity of Makran, a bimodal subduction zone, SE Iran ». Journal of Asian Earth Sciences 169 (janvier 2019) : 139–61. http://dx.doi.org/10.1016/j.jseaes.2018.08.009.
Texte intégralThèses sur le sujet "Makran (Iran)"
Pokharel, Shankar Babu. « Remote Sensing and GIS Analysis of Spatial Distribution of Fracture Patterns in the Makran Accretionary Prism, Southeast Iran ». Digital Archive @ GSU, 2007. http://digitalarchive.gsu.edu/geosciences_theses/8.
Texte intégralRegard, Vincent. « Variations temporelle et spatiale de la transition subduction-collision : tectonique de la transition Zagros-Makran (Iran) et modélisation analogique ». Phd thesis, Aix-Marseille 3, 2003. http://tel.archives-ouvertes.fr/tel-00003777.
Texte intégralNinkabou, Dia. « Tectono-sedimentary and geodynamic evolution of the Makran Subduction Zone and the Gulf of Oman, from the Late Cretaceous to Present ». Electronic Thesis or Diss., Sorbonne université, 2021. http://www.theses.fr/2021SORUS581.
Texte intégralThe Makran subduction zone, located between the Arabian, Indian and Eurasian plates, is characterized by one of the largest accretionary prism of the world. This Cenozoic prism shows stark morphological differences from East to West, onshore and offshore. To assess the causes for these differences, offshore multichannel seismic data has been studied throughout the prism and the Gulf of Oman, allowing us to assess the evolution of the study area at the basin scale. Seismic tomography data was also studied across the region, providing insights into the subduction zone's lithospheric structure. The results show that the structure of the offshore prism is partly linked to Plio-Pleistocene surface processes due to its reworking. The western sector of the prism shows mainly a large accumulation of sediments in the shelf, compared to the eastern sector, where sediments are also routed to the trench by a turbiditic system. The deep structure of the subduction zone is characterized by a first subducting plate related to the Arabian plate, affected by a sub-horizontal tear. This tear is located west of a major transfer zone identified on the northern Oman margin, indicating a possible segmentation of the subducting plate. This tear may be responsible for forming a major olistostrome, which impacts the morphology of the onshore wedge. An additional subducting plate, related to the Indian plate, is located in the easternmost sector of the subduction zone
Shah-Hosseini, Majid. « Geomorphic evolution and coastal hazards along the Iranian coast of Makran ». Thesis, Aix-Marseille, 2014. http://www.theses.fr/2014AIXM3010.
Texte intégralIn this thesis we have two main goals: (i) to reconstruct the Holocene coastal evolution and relative sea-level changes using strandplains around the Chabahar and Pozm bays; and (ii) to evaluate coastal hazards (tsunami and extreme storms) along the Iranian coast of Makran using high-energy deposits. Since the mid-Holocene, the shoreline rimming the bays of Chabahar and Pozm has prograded ~5 km and formed extensive strandplains. We documented relative sea-level changes along four coast-normal profiles. Internal architecture of strandplain imaged using Ground Penetrating Radar (GPR). The sedimentology and stratigraphy of the coastal sequence were studied by coring and trenching. The highest paleo-coastline is located about 5 km inland and stands approximately 15 m above present sea level. Paleo-shorelines date back between 4800 and 270 years BP at respective distances of 5 km to 670 m from the active shoreline. The spatial position of the palaeo-coastlines demonstrates a fall in local sea level of around 15 m during the last ~4800 years. Event deposits attesting to high-energy waves have been studied in low-lying coast by study of Over-washed sandy and shelly marine sediment and on the rocky shore by study of displaced boulder deposits. We applied hydrologic models to estimate the height and inundation distance of exceptional waves. Our results demonstrate that no known or probable storm is capable of detaching and transporting the boulders. Tsunami waves 4 m in height are enough to transport the boulders. We conclude the Makran coast has archived evidence of palaeo-tsunami events generated in the Makran subduction zone
Mutin, Benjamin. « Contribution à l'étude du peuplement des confins indo-iraniens au chalcolithique : caractérisation de la production céramique des périodes II et IIa du Makran pakistanais (4e millénaire avant J.-C.) ». Paris 1, 2007. http://www.theses.fr/2007PA010670.
Texte intégralBARBERO, EDOARDO. « Geological and petrological investigation of the western North Makran ophiolites (SE Iran) : new constraints for the Late Jurassic – Cretaceous tectono-magmatic and geodynamic evolution of the Neo-Tethys Ocean ». Doctoral thesis, Università degli studi di Ferrara, 2021. http://hdl.handle.net/11392/2488101.
Texte intégralIl Prisma di Accrezione del Makran (Iran meridionale) è legato alla convergenza tra la placca Araba e quella Euroasiatica, che è accomodata, a partire dal Cretacico, dalla subduzione verso Nord dell’oceano della Neo-Tetide. Nel dominio tettonico del North Makran sono preservate ofioliti mesozoiche, successioni sedimentarie e minori resti di rocce di derivazione continentale. La presente tesi è focalizzata sui complessi di Bajgan e Durkan, sull’unità di Band-e-Zeyarat e sul complesso di Ganj e comprende un dettagliato studio geologico di queste unità sul terreno così come un dettagliato studio geochimico-petrologico delle rocce magmatiche. Le unità studiate fanno parte del dominio del North Makran e sono state interpretate come i resti del bacino oceanico Mesozoico, noto in letteratura come Oceano del North Makran, e il suo margine continentale meridionale. Lo scopo di questa tesi è di presentare nuovi dati per meglio comprendere il significato geodinamico dei complessi di Bajgan e Durkan, dell’unità di Band-e-Zeyarat e del complesso di Ganj e vincolare l’evoluzione geodinamica dell’Oceano del North Makran. I dati presentati nella presente tesi documentano una complessa evoluzione tettono-magmatica per le diverse unità tettoniche. Il complesso di Ganj rappresenta una successione di arco vulcanico del Cretacico Superiore, probabilmente formatasi vicino alla placca Euroasiatica. L'ofiolite di Band-e-Zeyarat mostra un’architettura crostale, un’affinità geochimica delle rocce magmatiche e la composizione chimica delle fasi mineralogiche compatibile con la genesi in una dorsale medio oceanica durante il Cretacico Inferiore. I nuovi dati petrologici suggeriscono che l’ofiolite di Band-e-Zeyarat si sia formata durante l’interazione tra dorsale e plume di mantello. Il complesso di Durkan registra magmatismo alkalino coevo con sedimentazione pelagica e in ambiente di piattaforma carbonatica durante il Cretacico Superiore. La combinazione dei dati stratigrafici e petrologici indica che il Complesso di Durkan rappresenta i resti di una catena di seamounts deformata nel prisma di accrezione del Makran. Il complesso di Bajgan è costituito da meta-serpentiniti, varie tipologie di rocce metamorfiche da protoliti magmatici e rocce meta-sedimentarie. Questa tipologia di associazione litologica e la composizione chimica delle rocce magmatiche sono confrontabili con le ofioliti di tipo MOR (mid ocean ridge). Le datazioni di zirconi separati da meta-gabbri e meta-plagiograniti hanno fornito età comprese tra il Giurassico Superiore e il Cretacico Inferiore. I nuovi dati sul Complesso di Bajgan suggeriscono che corrisponda a un insieme di scaglie tettoniche di ofioliti Mesozoiche. I dati strutturali sull’ofiolite di Band-e-Zeyarat e il Complesso di Durkan indicano che queste unità hanno subito una storia deformativa polifasica tra il tardo Cretacico Superiore e il Paleocene-Eocene inferiore durante la loro accrezione e successiva esumazione nei settori frontali del prisma del Makran. In conclusione, i risultati della presente tesi forniscono importati vincoli per comprendere l’evoluzione geodinamica dell’Oceano del North Makran durante il tardo Giurassico e il Cretacico, così come il suo ruolo nella tettonica convergente attiva a partire dal tardo Cretacico Superiore. Il risultato principale è che i nuovi dati multidisciplinari suggeriscono che l’Oceano del North Makran rappresentasse un bacino oceanico maturo piuttosto che un bacino marginale o un back-arc come precedentemente suggerito in letteratura. Sono inoltre discusse le implicazioni dei nuovi dati nel contesto dell’evoluzione a scala regionale della Neo-Tetide durante il Cretacico.
Yamini, Fard Farzam. « Sismotectonique et structure lithosphérique de deux zones de transition dans le Zagros (Iran) : la zone de Minab et la zone de Qatar-Kazerun ». Phd thesis, Grenoble 1, 2003. http://tel.archives-ouvertes.fr/tel-00707751.
Texte intégralKarlsson, Simon. « Makten på Öland och i Möre : Järnålderns elit i ett lokalt perspektiv ». Thesis, University of Kalmar, School of Human Sciences, 2008. http://urn.kb.se/resolve?urn=urn:nbn:se:hik:diva-213.
Texte intégralThe social elite on Öland and in Möre in the south east of Sweden during the Iron Age is described on the basis of the archaelogical record, such as graves, settlements and traces of pre-Christian central places. The material is discussed to see if traces of an elite are to be found. The power configuration between Öland and Möre is also discussed.
Winbergh, Göran. « Elit och tvång, eller släkt och rådslag ? : Två tolkningar av makten på Gotland under romersk järnålder ». Thesis, Uppsala universitet, Institutionen för arkeologi och antik historia, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-391121.
Texte intégralMoore, Martyn Patrick John. « The Iron Age of the Makapan Valley area, central Transvaal ». Thesis, 2015. http://hdl.handle.net/10539/17046.
Texte intégralA culture-history research project was initiated for the relatively unresearched Makapan Valley area of the central Transvaal. The valley was surveyed intensively and fifty sites recorded. Three, 2429AA4 (Ficus), 2429AA24 (Kekane) and 2429AA36 were excavated. Ficus was a multicomponent site with four phases of occupation; an initial fifth to sixth century A.D. Lydenburg phase, a ninth to tenth century Eiland phase, an ambiguous fifteenth century entity and a superficial early twentieth century Ndebele occupation. This site sequence provided the framework for the research area's culture-history. Site 2429AA24 provided a larger sample of twentieth century Ndebele pottery. 2429AA36 proved sterile. The sample of excavated Eiland phase pottery has been significantly increased by the Ficus material.
Livres sur le sujet "Makran (Iran)"
Mardiyati, Umi. Peranan angkutan laut dalam penyediaan bahan makanan di Irian Jaya : Laporan penelitian. Jayapura : Jurusan Ekonomi, Fakultas Ilmu Sosial dan Ilmu Politik, Universitas Cenderawasih, 1993.
Trouver le texte intégralKjeldsen, Jens E., et Siri Meyer, dir. Krig, rett & ; retorikk – en bok om kommunikasjonsregimer. 3e éd. Retorikförlaget, 2004. http://dx.doi.org/10.52610/fhhn6728.
Texte intégralWahyudhi, Nostalgiawan, dir. Many Faces of Political Islam in the Middle East : Arah Baru Gerakan Politik Islam Pasca-Arab Spring. LIPI PRESS, 2020. http://dx.doi.org/10.14203/press.294.
Texte intégralChapitres de livres sur le sujet "Makran (Iran)"
Burg, J. P., A. Dolati, D. Bernoulli et J. Smit. « structural style of the Makran Tertiary accretionary complex in SE-Iran ». Dans Lithosphere Dynamics and Sedimentary Basins : The Arabian Plate and Analogues, 239–59. Berlin, Heidelberg : Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-30609-9_12.
Texte intégralDolati, A., et J. P. Burg. « Preliminary fault analysis and paleostress evolution in the Makran Fold-and-Thrust Belt in Iran ». Dans Lithosphere Dynamics and Sedimentary Basins : The Arabian Plate and Analogues, 261–77. Berlin, Heidelberg : Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-30609-9_13.
Texte intégralBarbero, Edoardo, Morteza Delavari, Asghar Dolati, Antonio Langone, Luca Pandolfi, Michele Marroni et Emilio Saccani. « New Geochemical and Age Data on the Bajgan Complex (Makran Accretionary Prism, SE Iran) : Implications for the Redefinition of Its Tectonic Setting of Formation from a Paleozoic Continental Basement to a Cretaceous Oceanic Domain ». Dans Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology and Petroleum Geology, 163–65. Cham : Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-43222-4_35.
Texte intégralSusilawati, Euis. « Pentingnya APSCO bagi Pembangunan Keantariksaan Indonesia ». Dans Kajian Kebijakan dan Informasi Kedirgantaraan, 116–32. Bogor : Mitra Wacana Media, 2015. http://dx.doi.org/10.30536/9786023181360.7.
Texte intégral« UPLIFTED MARINE TERRACES ALONG THE MAKRAN COAST OF PAKISTAN AND IRAN ». Dans Himalaya to the Sea, 225–46. Routledge, 2002. http://dx.doi.org/10.4324/9780203414637-27.
Texte intégralAubourg, C., B. Smith, H. Bakhtari, N. Guya, A. Eshragi, S. Lallemant, M. Molinaro, X. Braud et S. Delaunay. « Post-Miocene shortening pictured by magnetic fabric across the Zagros-Makran syntaxis (Iran) ». Dans Special Paper 383 : Orogenic curvature : Integrating paleomagnetic and structural analyses, 17–40. Geological Society of America, 2004. http://dx.doi.org/10.1130/0-8137-2383-3(2004)383[17:pspbmf]2.0.co;2.
Texte intégralPostma, Dirk Willem. « Kwetsbaar burgerschap : Naar een vrijplaats voor boeren, burgers en buitenlui ». Dans Geleefd Burgerschap : Van eenheidsdwang naar ruimte voor verschil en vitaliteit, 169–88. Uitgeverij SWP, 2012. http://dx.doi.org/10.36254/978-90-8850-334-4.10.
Texte intégralActes de conférences sur le sujet "Makran (Iran)"
Heidarzadeh, Mohammad, Moharram D. Pirooz, Nasser H. Zaker et Mohammad Mokhtari. « Modeling of Tsunami Propagation in the Vicinity of the Southern Coasts of Iran ». Dans ASME 2007 26th International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2007. http://dx.doi.org/10.1115/omae2007-29082.
Texte intégralGrando, Gianluca, et Ken McClay. « Subduction-related deformation processes in the Makran accretionary prism, offshore Iran ». Dans GEO 2008. European Association of Geoscientists & Engineers, 2008. http://dx.doi.org/10.3997/2214-4609-pdb.246.158.
Texte intégral« Probabilistic Tsunami Hazard of Splay and Normal Faults in the Western Makran/Iran ». Dans The Second Eurasian RISK-2020 Conference and Symposium. AIJR Publisher, 2020. http://dx.doi.org/10.21467/abstracts.93.2.
Texte intégralKhiabani Moghadam, Arash. « GEOCHEMISTRY AND PETROLOGY OF GABBRO INTRUSIONS AND ULTRAMAFIC ROCKS FROM WESTERN MARGIN OF MAKRAN ACCRETIONARY WEDGE (COLOURED MELANGE) COMPLEX, SE IRAN ». Dans GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-348921.
Texte intégralDafrina, Armelia, Deassy Siska et Maulana Hakiki. « Identifikasi Pengaruh Arsitektur Timur Tengah pada Desain Masjid Raya Pase Panton Labu ». Dans Temu Ilmiah IPLBI 2021. Ikatan Peneliti Lingkungan Binaan Indonesia, 2021. http://dx.doi.org/10.32315/ti.9.i023.
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