Results 11 to 20 of about 184 (170)

TSUNAMI RISK ASSESSMENT MODELLING IN CHABAHAR PORT, IRAN [PDF]

open access: yesThe International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, 2017
The well-known historical tsunami in the Makran Subduction Zone (MSZ) region was generated by the earthquake of November 28, 1945 in Makran Coast in the North of Oman Sea.
M. R. Delavar   +3 more
doaj   +1 more source

Geomorphological and Geochemical Characteristics Mud Volcanoes Near Zendan Fault ,Iran [PDF]

open access: yesSustainable Earth Trends, 2022
Mud volcanism is a global phenomenon usually associated with compressional tectonics that favor extrusion of fluid- and clay mineral-rich sediment both on land and offshore.
Keramat Nezhad Afzali
doaj   +1 more source

Simultaneous employment of hydrodynamical simulation and RS imageries for analyzing the influence of an anthropogenic construction on shoreline transformation [PDF]

open access: yesJournal of Hydraulic Structures, 2023
Coastal areas are usually heavily exploited. Numerous anthropogenic constructions are developed along the coastal areas for recreational, economic and/or cultural purposes. They influence the coastal hydrodynamics.
Danial Ghaderi, Maryam Rahbani
doaj   +1 more source

New geographical record and morphological features of the Indo‑Pacific tropical sand goby, Favonigobius reichei (Bleeker, 1854) from Iranian coast of the Makran Sea (Teleostei, Gobiidae) [PDF]

open access: yesCheck List, 2017
The Indo-Pacific tropical sand goby, Favonigobius reichei (Bleeker, 1854), is a gobiid fish native to estuarine and marine waters of the coasts of the Indian and the western Pacific Oceans. Four specimens of F.
Reza Sadeghi   +3 more
doaj   +3 more sources

Analysis of the Makran Coastline of Iran’s Vulnerability to Global Sea-Level Rise

open access: yesJournal of Marine Science and Engineering, 2021
The SE coast of Iran is of great economic and environmental importance. Global climate change affects this coastline through sea level rise (SLR), compounded by a decrease in sediment budgets in coastal areas. This study developed a Coastal Vulnerability
Ezatollah Ghanavati   +2 more
doaj   +1 more source

Microearthquakes and crustal structure off the Makran coast of Iran

open access: yesDeep Sea Research Part B. Oceanographic Literature Review, 1980
On the basis of bathymetric and seismic data collected recently off the coast of Makran in the Gulf of Oman, it has been suggested that the folding of the sediments at the northern edge of the abyssal plain is taking place at the present time. The folding is thought to be the consequence of ongoing subduction of the Arabian plate beneath the Eurasian ...
M. Niazi, H. Shimamura, M. Matsu’ura
openaire   +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   +1 more source

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

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   +1 more source

Stochastic Analysis of Tsunami Hazard of the 1945 Makran Subduction Zone Mw 8.1–8.3 Earthquakes

open access: yesGeosciences, 2020
Historical records of major earthquakes in the northwestern Indian Ocean along the Makran Subduction Zone (MSZ) indicate high potential tsunami hazards for coastal regions of Pakistan, Iran, Oman, and western India.
Payam Momeni   +3 more
doaj   +1 more source

Extension at the coast of the Makran subduction zone (Iran)

open access: yesTerra Nova, 2019
AbstractIn the Makran subduction zone, earthquake focal mechanisms and geodetic data indicate that the deforming prism currently experiences N–S compression. However, palaeostress inversions performed on normal faults observed along the coast reveal local stress components consistent with N‐S extension.
Normand, Raphaël   +2 more
openaire   +4 more sources

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