flysch – iranshahr – makran-structure-penci

Makran subduction zone, along the southern coasts of Iran and Pakistan, has a wide potential seismogenic zone may be capable generating large magnitude (M ~ 9) tsunamigenic earthquakes. Considering ambiguities exist in source characterization for megathrusts like Makran, where detailed geologic, seismic, geodetic data are insufficient, probabilistic tsunami hazard analysis (PTHA) is most preval...

There is a high rate of casualty among miners in the world every year. One way to reduce accidents and increase safety mines use risk management process identify respond major hazards mines. The present study an attempt investigate assessment risks Faryab chromite underground In this paper, method AHP type-1 type-2 fuzzy sets used for assessment. Upon studying two (Makran Nemat), 45 were divide...

Atarbolana makranensis sp. n. is described from the intertidal zone of Makran along the Iranian coast of the Gulf of Oman. Atarbolana makranensis sp. n. can be recognized by the presence of a tuft of long setae on the antennal flagellum of males, elongate pleotelson with 12 robust marginal setae, pleotelson with narrowly rounded apex extending well beyond the uropodal endopod, uropodal endopod ...

The Makran coast is extremely vulnerable to tsunamis and earthquakes due to the presence of three very active tectonic plates namely, the Arabian, Eurasian and Indian plates. On 28 November 1945 at 21:56 UTC, a massive Makran earthquake generated a destructive tsunami in the Northern Arabian Sea and the Indian Ocean. The tsunami was responsible for loss of life and great destruction along the c...