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...

The evolution of the western Mediterranean of an 'interna1 zone plate' by the mechanism basin is considered. The Provence basin invoked by Karig. Lower or middle Miocene results from the Oligocene migration of Conica squeezing of the interna1 zones against the and Sardinia southeastwards. The North North Afncan platform caused ejection of the African basin was created by the dislocation flysch ...

The Chugach-Prince William (CPW) terrane is an Upper Cretaceous to Eocene accretionary complex exposed for ~2200 km in southern Alaska, extending from Baranof Island in the east to Sanak Island in the west. One of the thickest subduction-related accretionary complexes in the world, the CPW terrane is composed of deep-water flysch and associated volcanic rocks and is intruded by near-trench plut...

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 ...

conclusion based on the results, the vectors of cutaneous leishmaniasis include of p. papatasi, p. salehi, p. sergenti and moreover the vectors of visceral leishmaniasis include of p. keshishiani and p. alexandri have been found. materials and methods sand flies were collected by using sticky traps from selected villages (outdoors as well as indoors). traps were fixed at sundown and sand flies ...