makran subduction zone (msz) offshore of iran and pakistan is one of the most tsunamigenic sources in the indian ocean. historically, the msz has generated some tsunamigenic earthquakes like that of 28 november 1945 with the death tool of more than 4000 people along the coasts of iran, pakistan, india, and oman. in this study, the tsunami hazard associated with the msz is investigated. at first...

The Makran region, which borders southern Iran and Pakistan along the Gulf of Oman, has experienced multiple tsunamis in last century, with some being triggered by submarine landslides. However, role played landslides been largely neglected tsunami hazard assessments western Makran. In present study, four different landslide scenarios volumes 10–40 km3 are simulated on 25 locations Makran, resu...

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...

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 ...

Extreme coastal inundation associated with the 2004 Indian Ocean and 1945 Makran tsunamigenic-earthquakes highlight the risk of tsunamis to coastlines of the northern Oman Sea. Foraminifera have been used as indicators of paleotsunamis in the past where allochthonous tests, found in low-energy environments such as in coastal lagoons, ponds, and marshes, indicate marine overwash. In this study, ...

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...