نتایج جستجو برای: central iran zone

تعداد نتایج: 669412  

Journal: :Mongolian Journal of International Affairs 2015

Journal: :Journal of Applied Sciences 2008

Journal: :International Journal of Infectious Diseases 2008

2011
A. Eslami R. Nabavi H. R. Shokrani S. Bokaie P. Shayan D. Saadati

Gastrointestinal nematodes of small ruminants are one of the major causes of productivity loss.This study was carried out to determine the correlation between the prevalence, seasonal incidence and geographical distribution January 12, 2011of abomasal worm infection of native sheep in 3 different climatic zones of Iran, suitable for animal husbandry. From March 2008 to February 2009 the content...

Journal: :journal of tethys 0

there are three different basic dykes in the northeast of golpayegan area, central part of sanandaj-sirjan zone (ssz) including: mylonitic gabbros (group 1), alkali dioritic-basanitic dykes (group 2) and alkali monzogabbroic to monzodioritic dykes (group 3). group 2 and 3 cut post-collisional rocks and are related to after subduction processes of neo-tethys. geochemistry characteristic of studi...

2010
Vahid Noaman Parviz Shayan

Anaplasma bovis is a leukocytotropic agent of bovine anaplasmosis and there is no available information about molecular study on this agent in cattle of Iran. In this study a total 150 cattle blood samples were collected from central part of Iran. The presence of A. bovis examined using light microscopic detection and species-specific nested polymerase chain reaction (nested-PCR) based on 16S r...

M Mahdavi

A sequence of Permian rocks crops out in Northwest of Khur in Central Alborz, North of Iran. This sequence consists of the Dorud (Asselian-Sakmarian), Ruteh (Artinskian-Murgabian) and Nesen (Early Djulfian) formations. The Ruteh and Nesen formations in Alborz Range were deposited in a shallow marine environment of the continental margin in the Paleo-Tethys. The Ruteh Formation with a thickness ...

Journal: :Tectonophysics 2021

Tectonic stresses governed by the Arabia – Central Iran collision are transferred throughout Iranian Plateau. The orientation of maximum horizontal stress (σ 1 ) significantly changes (~90°) in Persian block NW Iran. However, exact spatial extent and boundary conditions for these poorly defined. This study investigates late Cenozoic regime a key region including Mahneshan Mianeh Basin (MMCB), G...

2012
Touraj Banirostam Kamal Mirzaie Mehdi N. Fesharaki

Touraj Banirostam, Kamal Mirzaie, Mehdi N. Fesharaki Department of Computer Engineering, Central Tehran Branch, Islamic Azad University, IRAN Email: [email protected] Department of Computer Engineering, Maybod Branch, Islamic Azad University, IRAN Email: [email protected] Department of Computer Engineering, Science and research Branch, Islamic Azad University, IRAN Email: fesharak...

Afshin Ashja Ardalan Elham Shah Hosseini Mohammad Hossein Razavi Mohammad Hashem Emami

The area of study is located 120 Km north-east of Shahrood city. In terms of structure and geological classification, this area is located in the northern part of central Iran zone. Granitoids of Troud ranging from monzonite to granite. The main minerals of granitoids are quartz, plagioclase, and orthose. The accessory minerals are biotite, hornblende, sphene, and opaque minerals. Various textu...

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