Results 11 to 20 of about 173 (150)

Holocene Sedimentary Record and Coastal Evolution in the Makran Subduction Zone (Iran) [PDF]

open access: yesQuaternary, 2019
The western Makran coast displays evidence of surface uplift since at least the Late Pleistocene, but it remains uncertain whether this displacement is accommodated by creep on the subduction interface, or in a series of large earthquakes.
Raphaël Normand   +4 more
doaj   +4 more sources

Subduction thermal state, slab metamorphism, and seismicity in the Makran Subduction Zone

open access: yesEarth and Planetary Physics
The dependence of the subduction regime on three-dimensional slab geometry poses a challenge for accurately estimating the evolving thermal structure of megathrusts globally.
Haris Faheem   +5 more
doaj   +2 more sources

Dating and morpho-stratigraphy of uplifted marine terraces in the Makran subduction zone (Iran) [PDF]

open access: yesEarth Surface Dynamics, 2019
The western part of the Makran subduction zone (Iran) is currently experiencing active surface uplift, as attested by the presence of emerged marine terraces along the coast.
R. Normand   +5 more
doaj   +6 more sources

Seismicity and return period investigation of destructive earthquake in Makran subduction zone

open access: yesDiscover Geoscience
This work uses the frequency-magnitude relation for the earthquakes to analyze seismicity and return period for the earthquakes in Makran subduction and its adjacent region. The data for seismicity analysis and return period range from 1934 to 2022, with
Adil Rehman, Huai Zhang
doaj   +2 more sources

Tsunami hazard assessment in the Makran subduction zone [PDF]

open access: yesNatural Hazards, 2020
17 pages, 9 figures, 1 table. Other author's papers can be downloaded at http://www.denys-dutykh.com/
Amin Rashidi   +3 more
openaire   +3 more sources

Deformational pattern and seismogenic potential of the eastern Makran subduction zone [PDF]

open access: yesJournal of Asian Earth Sciences, 2022
In last 500 years, the ∼900 km long Makran subduction zone (MSZ) has hosted 9 M7+ large earthquakes, and 8 of them activated the eastern segment of the fault. The 1945 M 8.1 megathrust event also generated significant tsunami signifying the region as active subduction zone in the world.
Parvaiz, Shaukat   +3 more
openaire   +1 more source

New Constraints for the On‐Shore Makran Subduction Zone Crustal Structure [PDF]

open access: yesJournal of Geophysical Research: Solid Earth, 2022
AbstractThe Makran Subduction Zone is the primary seismic/tsunami hazard of the northwestern Indian Ocean, but little is known of its on‐shore seismic structure. We derived a shear wave velocity model extending to 100 km depth beneath a ∼400 km‐long seismic profile oriented parallel to the convergence vector of the Arabian Sea Plate.
Priestley, Keith   +6 more
openaire   +1 more source

Probabilistic tsunami hazard assessment for the Makran region with focus on maximum magnitude assumption [PDF]

open access: yesNatural Hazards and Earth System Sciences, 2016
Despite having been rather seismically quiescent for the last decades, the Makran subduction zone is capable of hosting destructive earthquakes and tsunami.
A. Hoechner, A. Y. Babeyko, N. Zamora
doaj   +1 more source

Quaternary Thrusting in the Central Oman Mountains—Novel Observations and Causes: Insights from Optical Stimulate Luminescence Dating and Kinematic Fault Analyses

open access: yesGeosciences, 2020
For the first time, Quaternary thrusts are documented within the Central Oman Mountains to the northwest of the Jabal Akhdar Dome. Thrusts with a throw of up to 1.1 m displace Quaternary alluvial fan conglomerates.
Daniel Moraetis   +4 more
doaj   +1 more source

THE 326 BC EARTHQUAKE AND TSUNAMI IN THE NORTHERN ARABIAN SEA - IMPACT ON THE FLEET OF ALEXANDER THE GREAT [PDF]

open access: yesScience of Tsunami Hazards, 2022
Ancient Greek and Indian texts support that destructive sea waves along the Makran coast in the northern Arabian Sea were responsible for the partial destruction of Alexander the Great’s fleet in 326 BC.
George Pararas-Carayannis
doaj  

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