Results 31 to 40 of about 1,658 (164)
Main drivers of drainage pattern development in onshore makran accretionary wedge, se Iran
Over time, river networks achieve a specific pattern as determined by the function of several factors such as climate, tectonic, geological structures, topography, lithology, and base-level fluctuations.
Sarıkaya, Mehmet Akif +5 more
core +1 more source
Halal Tourism and Sustainable Development in Makran [PDF]
In recent decades, the tourism industry has emerged as one of the most significant catalysts for economic growth and social development worldwide.
Mohammad Ali Khaliji
doaj +1 more source
TSUNAMI RISK ASSESSMENT MODELLING IN CHABAHAR PORT, IRAN [PDF]
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
New geographical record of the lined rockskipper, Istiblennius lineatus (Valenciennes, 1836) from the Iranian coast of the Makran Sea (Teleostei, Blenniidae) [PDF]
The lined rockskipper, Istiblennius lineatus, is a species of combtooth blenny fish distributed from the Laccadive and Maldive islands, central Indian Ocean, east to Mangareva and Gambier Islands in the Pacific Ocean.
Hamid Reza Mehraban, Hamid Reza Esmaeili
doaj +3 more sources
Abstract We present heat flow estimates beneath the forearc slopes off Hyuga‐nada and Cape Muroto in the Nankai Trough, where the Philippine Sea plate subducts beneath the southwestern Japan. Using seismic reflection data, we identified Bottom Simulating Reflectors and derived heat flow ranging from 20 to >140 mW/m2.
Masataka Kinoshita +4 more
wiley +1 more source
Depositional environments, provenance and tectonic settings of Ispikan group exposed in south west Makran, were revealed by lithofacies, petrography and geochemistry studies.
Muhammad Ahmed Farooqui +4 more
doaj +1 more source
Abstract The Cenozoic topographic growth of the Iranian Plateau, situated at the Arabia‐Eurasia collision front, provides insights into continental collision dynamics. However, the relative contributions of tectonic shortening versus deep mantle processes to crustal thickening remain debated because systematic quantitative constraints on paleo‐crustal ...
Jun Hu +4 more
wiley +1 more source
Late Campanian (74–71 Ma) Arabia–Eastern Anatolia Collision and Its Geodynamic Implications
Abstract The East Anatolian Plateau is a major collisional feature within the Tethyan realm formed as a late‐stage result of the collision between East Anatolia and the Arabian Platform. The timing of this collision is highly debated, with estimates from the Late Cretaceous to the Miocene.
Remziye Akdoğan +7 more
wiley +1 more source
Probabilistic tsunami hazard assessment for the Makran region with focus on maximum magnitude assumption [PDF]
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
The evolution of pore fluid pressure ( Pf$P_{\mathrm{f}}$) in the most seaward portion of a subduction accretionary prism plays an essential role in the cycle of tsunamigenic earthquakes. Based on recent geophysical observations, here we propose a testable conceptual model for this evolution for northern Cascadia offshore of Washington.
Tianhaozhe Sun, Kelin Wang
wiley +1 more source

