Literatura científica selecionada sobre o tema "Subduction – Makran (Iran)"
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Artigos de revistas sobre o assunto "Subduction – Makran (Iran)"
Haberland, Christian, Mohammad Mokhtari, Hassan Ali Babaei, Trond Ryberg, Mehdi Masoodi, Abdolreza Partabian e Jörn Lauterjung. "Anatomy of a crustal-scale accretionary complex: Insights from deep seismic sounding of the onshore western Makran subduction zone, Iran". Geology 49, n.º 1 (13 de agosto de 2020): 3–7. http://dx.doi.org/10.1130/g47700.1.
Texto completo da fonteSafari, A., A. M. Abolghasem, N. Abedini e 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 de setembro de 2017): 523–29. http://dx.doi.org/10.5194/isprs-archives-xlii-4-w4-523-2017.
Texto completo da fonteRashidi, Amin, Denys Dutykh, Zaher Hossein Shomali, Nasser Keshavarz Farajkhah e Mohammadsadegh Nouri. "A Review of Tsunami Hazards in the Makran Subduction Zone". Geosciences 10, n.º 9 (18 de setembro de 2020): 372. http://dx.doi.org/10.3390/geosciences10090372.
Texto completo da fonteHafeez Abbasi, Muhammad Imran. "IS MAKRAN A SEPARATE MICROPLATE? A SHORT REVIEW". MALAYSIAN JOURNAL OF GEOSCIENCES 5, n.º 1 (19 de novembro de 2020): 01–05. http://dx.doi.org/10.26480/mjg.01.2021.01.05.
Texto completo da fonteNormand, Raphaël, Guy Simpson e Abbas Bahroudi. "Extension at the coast of the Makran subduction zone (Iran)". Terra Nova 31, n.º 6 (30 de julho de 2019): 503–10. http://dx.doi.org/10.1111/ter.12419.
Texto completo da fonteNormand, Raphaël, Guy Simpson, Frédéric Herman, Rabiul Haque Biswas e Abbas Bahroudi. "Holocene Sedimentary Record and Coastal Evolution in the Makran Subduction Zone (Iran)". Quaternary 2, n.º 2 (12 de junho de 2019): 21. http://dx.doi.org/10.3390/quat2020021.
Texto completo da fonteHoechner, Andreas, Andrey Y. Babeyko e Natalia Zamora. "Probabilistic tsunami hazard assessment for the Makran region with focus on maximum magnitude assumption". Natural Hazards and Earth System Sciences 16, n.º 6 (10 de junho de 2016): 1339–50. http://dx.doi.org/10.5194/nhess-16-1339-2016.
Texto completo da fonteHoechner, A., A. Y. Babeyko e N. Zamora. "Probabilistic tsunami hazard assessment for the Makran region with focus on maximum magnitude assumption". Natural Hazards and Earth System Sciences Discussions 3, n.º 9 (1 de setembro de 2015): 5191–208. http://dx.doi.org/10.5194/nhessd-3-5191-2015.
Texto completo da fonteNemati, Majid. "Seismotectonic and seismicity of Makran, a bimodal subduction zone, SE Iran". Journal of Asian Earth Sciences 169 (janeiro de 2019): 139–61. http://dx.doi.org/10.1016/j.jseaes.2018.08.009.
Texto completo da fonteNormand, Raphaël, Guy Simpson, Frédéric Herman, Rabiul Haque Biswas, Abbas Bahroudi e Bastian Schneider. "Dating and morpho-stratigraphy of uplifted marine terraces in the Makran subduction zone (Iran)". Earth Surface Dynamics 7, n.º 1 (26 de março de 2019): 321–44. http://dx.doi.org/10.5194/esurf-7-321-2019.
Texto completo da fonteTeses / dissertações sobre o assunto "Subduction – Makran (Iran)"
Ninkabou, 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.
Texto completo da fonteThe 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
Regard, 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.
Texto completo da fonteTrabalhos de conferências sobre o assunto "Subduction – Makran (Iran)"
Heidarzadeh, Mohammad, Moharram D. Pirooz, Nasser H. Zaker e Mohammad Mokhtari. "Modeling of Tsunami Propagation in the Vicinity of the Southern Coasts of Iran". In ASME 2007 26th International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2007. http://dx.doi.org/10.1115/omae2007-29082.
Texto completo da fonteGrando, Gianluca, e Ken McClay. "Subduction-related deformation processes in the Makran accretionary prism, offshore Iran". In GEO 2008. European Association of Geoscientists & Engineers, 2008. http://dx.doi.org/10.3997/2214-4609-pdb.246.158.
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