Bibliografías temáticas / Makran subduction

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Literatura académica sobre el tema "Makran subduction"

Autor: Grafiati
Publicado: 25 de mayo de 2024
Última modificación: 31 de julio de 2025

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Artículos de revistas sobre el tema "Makran subduction"

1

Ghadimi, Homa, Alireza Khodaverdian, and Hamid Zafarani. "Active deformation in the Makran region using geological, geodetic and stress direction data sets." Geophysical Journal International 235, no. 3 (2023): 2556–80. http://dx.doi.org/10.1093/gji/ggad393.

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SUMMARY Neotectonic flow of the Makran subduction zone is estimated using a kinematic modelling technique based on iterated weighted least-squares that fits to all kinematic data from both geological and geophysical sources. The kinematic data set includes 87 geodetic velocities, 1962 principal stress directions, 90 fault traces, 56 geological heave rates and velocity boundary conditions. Low seismicity of western Makran compared to its eastern part, may indicate that either the subduction interface is currently locked, accumulating elastic strain or aseismic slip (creep) occurs along this par
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2

Haberland, Christian, Mohammad Mokhtari, Hassan Ali Babaei, et al. "Anatomy of a crustal-scale accretionary complex: Insights from deep seismic sounding of the onshore western Makran subduction zone, Iran." Geology 49, no. 1 (2020): 3–7. http://dx.doi.org/10.1130/g47700.1.

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Abstract The Makran subduction zone has produced M 8+ earthquakes and subsequent tsunamis in historic times, hence indicating high risk for the coastal regions of southern Iran, Pakistan, and neighboring countries. Besides this, the Makran subduction zone is an end-member subduction zone featuring extreme properties, with one of the largest sediment inputs and the widest accretionary wedge on Earth. While surface geology and shallow structure of the offshore wedge have been relatively well studied, primary information on the deeper structure of the onshore part is largely absent. We present th
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3

Namdarsehat, Peyman, Wojciech Milczarek, Seyed-Hani Motavalli-Anbaran, and Matin Khaledzadeh. "Makran Subduction Zone: A Review and Synthesis." Geosciences 14, no. 8 (2024): 219. http://dx.doi.org/10.3390/geosciences14080219.

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This review synthesizes existing research to elucidate the factors driving the distinct tectonic behaviors in the western and eastern Makran subduction zone, focusing on seismic activity, uplift rate, convergence rate, coupling, and subduction angle. The literature identifies the asymmetry in pressure and the variation in subduction angles between the western and eastern parts of the Makran as key factors in defining the region’s tectonic patterns. The western region has a steeper subduction angle, resulting in lower pressure, reduced coupling, and decreased seismic activity. This disparity ar
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Safari, A., A. M. Abolghasem, N. Abedini, and 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 (September 27, 2017): 523–29. http://dx.doi.org/10.5194/isprs-archives-xlii-4-w4-523-2017.

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Makran subduction zone is one of the convergent areas that have been studied by spatial geodesy. Makran zone is located in the South Eastern of Iran and South of Pakistan forming the part of Eurasian-Arabian plate's border where oceanic crust in the Arabian plate (or in Oman Sea) subducts under the Eurasian plate ( Farhoudi and Karig, 1977). Due to lack of historical and modern tools in the area, a sampling of sparse measurements of the permanent GPS stations and temporary stations (campaign) has been conducted in the past decade. Makran subduction zone from different perspectives has unusual
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Rashidi, Amin, Denys Dutykh, Zaher Hossein Shomali, Nasser Keshavarz Farajkhah, and Mohammadsadegh Nouri. "A Review of Tsunami Hazards in the Makran Subduction Zone." Geosciences 10, no. 9 (2020): 372. http://dx.doi.org/10.3390/geosciences10090372.

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The uncertain tsunamigenic potential of the Makran Subduction Zone (MSZ) has made it an interesting natural laboratory for tsunami-related studies. This study aims to review the recent activities on tsunami hazard in the Makran subduction zone with a focus on deterministic and probabilistic tsunami hazard assessments. While almost all studies focused on tsunami hazard from the Makran subduction thrust, other local sources such as splay faults and landslides can be also real threats in the future. Far-field tsunami sources such as Sumatra-Andaman and Java subduction zones, commonly lumped as th
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Lodhi, Hira Ashfaq, Shoaib Ahmed, and Haider Hasan. "Tsunami heights and limits in 1945 along the Makran coast estimated from testimony gathered 7 decades later in Gwadar, Pasni and Ormara." Natural Hazards and Earth System Sciences 21, no. 10 (2021): 3085–96. http://dx.doi.org/10.5194/nhess-21-3085-2021.

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Abstract. The towns of Pasni and Ormara were the most severely affected by the 1945 Makran tsunami. The water inundated land for almost 1 km at Pasni, engulfing 80 % of the huts of the town, while at Ormara the tsunami inundated land for 2.5 km, washing away 60 % of the huts. The plate boundary between the Arabian Plate and Eurasian Plate is marked by Makran subduction zone (MSZ). This Makran subduction zone in November 1945 was the source of a great earthquake (8.1 Mw) and an associated tsunami. Estimated death tolls, waves arrival times, and the extent of inundation and runup have remained v
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Rehman, Adil, and Huai Zhang. "Generalized Extreme Value Distribution for Modeling Earthquake Risk in Makran Subduction Zone Using Extreme Value Theory." Indonesian Journal of Earth Sciences 3, no. 2 (2023): A819. http://dx.doi.org/10.52562/injoes.2023.819.

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The long-term pattern of severe incidents is one of the most crucial and fascinating topics of seismic events. This work aims to analyze the maximum annual earthquake magnitude in the Makran subduction zone using extreme value theory by implementing the block maxima method. The seismic data utilized for the current study was collected from the International Seismological Center (ISC) ranging from 1934 to 2022. The extreme parameters have fitted utilizing the generalized extreme value distribution. Numerous plots of the generalized extreme value distribution approach gave the accuracy of the us
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Faheem, Haris, YingFeng Ji, WeiLing Zhu, Rui Qu, Ye Zhu, and Shoichi Yoshioka. "Subduction thermal state, slab metamorphism, and seismicity in the Makran Subduction Zone." Earth and Planetary Physics 9, no. 2 (2025): 1–13. https://doi.org/10.26464/epp2025004.

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REHMAN, Adil, and Huai ZHANG. "Probabilistic forecast of next earthquake event in Makran subduction zone using Weibull distribution." Contributions to Geophysics and Geodesy 54, no. 1 (2024): 85–93. http://dx.doi.org/10.31577/congeo.2024.54.1.5.

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Earthquake is the most lethal type of natural disaster. Researchers have been working to develop precise earthquake prediction methods to save lives. A statistical investigation is an effective earthquake prediction method because they offer more details about the seismic risk or hazard issue. This study utilizes seismic data from the Makran subduction zone from 1934 to 2017. Probability distributions may be employed to assess the risk of seismic events and earthquake occurrence probability. This work estimates the probability of the next major event in the Makran subduction zone through Weibu
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Hafeez Abbasi, Muhammad Imran. "IS MAKRAN A SEPARATE MICROPLATE? A SHORT REVIEW." MALAYSIAN JOURNAL OF GEOSCIENCES 5, no. 1 (2020): 01–05. http://dx.doi.org/10.26480/mjg.01.2021.01.05.

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Makran Subduction Zone (MZS) is important as this region lies on both sides of the border of Iran and Pakistan along the coastline. Makran Subduction complex has pervasive seismicity and diverse focal mechanism solutions and being in the vicinity of Triple Junction where three major Tectonic plates; Arabian, Eurasian and Indian plates are connecting. Both of Chabahar and Gwadar ports are located in this vicinity, on which China is investing for CPEC, Belt and Road Initiative. The whole world is looking at these projects of Makran, as this may define and transform the future of trade. Hence Geo
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Tesis sobre el tema "Makran subduction"

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Mouchot, Nicolas. "Tectonique et sédimentation sur le complexe de subduction du Makran pakistanais." Cergy-Pontoise, 2009. http://biblioweb.u-cergy.fr/theses/09CERG0520_diff.pdf.

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Le complexe de subduction de Makran, au nord de la mer d’Arabie, à développé un vaste prisme d’accrétion en réponse à la subduction de la plaque Arabe sous la plaque Eurasie. Les différentes campagnes océanographiques, menées au large du Pakistan, ont révélé la morphologie et la configuration des structures des plaques plongeante et chevauchante. A partir du nouveau jeu de données acquis en 2004, j’évalue les implications des structures de la plaque plongeante sur la déformation dans le prisme mais également sur la cinématique de la région. Par ailleurs, grâce à la couverture quasiment continu
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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.

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La zone de subduction du Makran, situé entre les plaques Arabe, Indienne et Eurasienne est caractérisé par l’un des plus grands prisme d’accrétion au monde. D’âge cénozoïque, ce prisme présente de fortes différences dans sa morphologie d’Est en Ouest, à terre et en mer. Afin de déterminer les causes de ces disparités, des données de sismiques réflexion ont été étudiés en mer à travers le prisme et le Golfe d’Oman, nous renseignant sur l’évolution de la zone d’étude à l’échelle du bassin. Des données de tomographie sismique ont aussi été étudiés à travers la région, nous renseignant sur la stru
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Smith, Gemma Louise. "The structure, fluid distribution and earthquake potential of the Makran Subduction Zone, Pakistan." Thesis, University of Southampton, 2013. https://eprints.soton.ac.uk/359131/.

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The Makran subduction zone (offshore Pakistan and Iran) has the largest accretionary prism of any margin worldwide, formed due to the thick incoming sediment section of up to 7.5 km. This margin has been relatively understudied, and this thesis presents a new, detailed structural and hydrological interpretation and seismogenic hazard assessment for the Makran. The accretionary prism is dominated by simple, imbricate thrusts which form seaward verging, anticlinal ridges up to 200 km long. The prism has a low average taper angle of 4.5°. Two oceanic basement features intersect the deformation fr
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4

Pajang, Sepideh. "Short-term deformation of accretionary prism, the role of mechanical and thermal inheritance. Application to Makran." Electronic Thesis or Diss., Sorbonne université, 2021. http://www.theses.fr/2021SORUS483.

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Les données GPS indiquent que la subduction accumule des contraintes qui devraient être libérées lors de futurs séismes, Makran potentiel sismogénique est très mal contraint. J’ai d’abord construit une carte structurale le long de la partie iranienne de la mer d'Oman. Ensuite, j’ai contraint la pression de fluide interstitiel et les propriétés de friction du prisme à partir de la théorie du prisme critique et de l'analyse limite. Les résultats montrent que le long des profils Est et Ouest, une transition d'une friction très faible à une friction extrêmement faible est nécessaire pour activer l
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5

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.

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Les transitions spatiale et temporelle de la subduction à la collision sont des charnières géodynamiques. Nous précisons dans ce travail le rôle et le devenir de ces zones grâce à des modèles analogiques et l'étude tectonique d'un cas réel. La modélisation a montré qu'une transition temporelle entre subduction et collision est toujours marquée par une phase de subduction continentale. La durée de cette phase dépend de la façon dont se déforme la lithosphère subductée en profondeur. Plus elle se déforme, plus courte est la subduction continentale. Dans le cas d'une transition latérale entre sub
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Capítulos de libros sobre el tema "Makran subduction"

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Mupparthi, Praveen, G. Jai Shankar, and Kirti Srivastava. "Comparison of Tsunami Arrival Times Using GIS Methods: A Case Study in the Makran Subduction Zone, West Coast of India." In Springer Series in Geomechanics and Geoengineering. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-77276-9_63.

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2

Asgharzadeh, Parisa, Shutian Ma, and Darioush Motazedian. "Further Studies on Three Large Earthquakes in the Makran Subduction Zone Region: The Crustal Velocity and Source Rupture Models." In Advances in Earthquake Research and Engineering [Working Title]. IntechOpen, 2024. https://doi.org/10.5772/intechopen.1007812.

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Three large earthquakes (2011-01-18 Pakistan Mw 7.2; 2013-04-16 IRAN Mw 7.7; and 2013-09-24 Pakistan Mw 7.8) occurred in the Makran subduction zone north region. This chapter introduces an average crustal model retrieved using Rayleigh wave dispersion data in the three earthquake region and their vicinity, the source rupture modeling results, and some geological background features. The centers of the major ruptures of the 2011 Mw 7.2 and the 2013 Mw 7.7 earthquakes were at depth about 65 km; the major rupture of the shallow 2013 Mw 7.8 earthquake was within the upper crust. The focal mechanis
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Actas de conferencias sobre el tema "Makran subduction"

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Heidarzadeh, Mohammad. "Far-Field Effects of Large Tsunamis Produced by the Makran Subduction Zone." In ASME 2009 28th International Conference on Ocean, Offshore and Arctic Engineering. ASMEDC, 2009. http://dx.doi.org/10.1115/omae2009-79362.

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The 2004 Indian Ocean tsunami which exported death and destruction to far distant shores, once more emphasized the tsunami hazards associated with transoceanic tsunamis. Historical records of tsunamis in the Makran subduction zone (MSZ) reveal that Makran tsunamis are capable of producing large waves in the far-field. The Makran tsunami of 1945 produced by an Mw8.1 earthquake was reported to cause far-field effects in the Indian Ocean and reached a height of about 30 cm in the Seychelles, at the distance of about 3500 km from the MSZ. Here, we assess historical observations of this event and p
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2

Heidarzadeh, Mohammad, Moharram D. Pirooz, Nasser H. Zaker, and 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.

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The extensive death toll and sever economical damages brought by the 2004 Indian Ocean tsunami has emphasized the urgent need for assessing the hazard of tsunami in this ocean, and determining the most vulnerable coastlines to the impact of possible tsunami. In this paper the hazard of tsunami for southern coasts of Iran bordering the Indian Ocean is discussed. At first, historical data of tsunami occurrences on the Iranian southern coasts are collected, described and analyzed. Then, numerical simulation of potential tsunamis in the Makran subduction zone is performed and the tsunami wave heig
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Grando, Gianluca, and 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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Pezzopane, Silvio, and John Whitney. "A SEISMOTECTONIC REVIEW OF THE IMPACT OF THE MAKRAN SUBDUCTION ZONE ON THE HELMAND-SISTAN BLOCK." In Cordilleran Section - 119th Annual Meeting - 2023. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023cd-387366.

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