نتایج جستجو برای: binalud and robat

تعداد نتایج: 16827180  

Journal: :مطالعات باستان شناسی 0
مهران مقصودی دانشیار گروه جغرافیای طبیعی دانشگاه تهران سید محمد زمانزاده استادیار گروه جغرافیای طبیعی دانشگاه تهران اصغر نویدفر دانشجوی دکتری ژئومورفولوژی دانشگاه تهران روح الله یوسفی زشک استادیار گروه باستا ن شناسی دانشگاه آزاد ورامین حجت الله احمدپور دانش آموختۀ کارشناسی ارشد باستان شناسی دانشگاه آزاد ورامین

the ancient hills are the human’s close and far activities sense. these places may be the transit camp survivors or ruins towns or villages. this paper studies the archaeology of the ancient hill of meymanabad using micromorphology methods. this hill situated in robat kareem_in south-east village called meymantabad. the result has showed that before the establishment of the site occupations the...

Journal: :journal of tethys 0

asmari formation was deposited in the foreland zagros basin (southwest iran). in this research, biostratigraphy related to the asmari formation in north of khorram abad, robat namaki section, is discussed. in the studied stratigraphic section, the asmari formation overlies the shahbazan formation and underlies gachsaran formation and consists of cream to gray medium to thick limestone and marl....

Mashhad Plain affects by a series of active faults in the northern margin of the Binalud and the southern margin of the Kopet-Dagh mountain ranges. The activity of these faults forms the morphology of the stepped bedrock of the Plain. In addition, the faults’ activities in the Quaternary period are the main effective parameters in thickness and texture of aquifer deposits in Mashhad Plain. In t...

Journal: :جغرافیا و توسعه ناحیه ای 0
علی کیوان زراعتکار بهنام رحیمی

the sangbast-shandiz fault zone, with a length of about 57 km, a width of moderately 2 km, and a nw-se direction, is located about 15 km in the west of mashhad city. that is one of the major faults in the binalud mountains. geomorphic evidences illustrate that the sangbast-shandiz fault zone has dextral strike- slip offsets with thrust activity. in this article, we investigated geomorphic featu...

H Nikoopour, M Amin, MR Fazeli,

Background: Plant extracts and essential oils are commonly used in traditional and industrial doogh products to inhibit bacterial activities. Objective: In this study, the antibacterial effects of the essential oils of Olivera decumbens and Nepeta binaludensis against Staphylococcus aureus and Escherichia coli in doogh were investigated. Methods: Essential oils of Olivera decumbens and Nepeta...

2012
M Yazdkhasti M Keshavarz ES Merghaati Khoei AF Hosseini S ESmaeilzadeh M Amiri Pebdani H Jafarzadeh

BACKGROUND Quality of life in post-menopausal women and menopausal symptoms are closely related concepts. Influence health education policy in order to promote health and adopt a menopause lifestyle requires alternative strategies, including health training programs with community - based interventions. The current study aims to survey the effects of support groups on quality of life of post-me...

ابراهیمی, خسرو , مظلومی, علیرضا , همام , سید مسعود , گرمابی, نازنین ,

Shelgerd area is located south of Mashhad, N.E of Iran, within Binalud Structural Zone. This region is affected by regional metamorphism, slate and phylite are the main metamorphic rocks of the area. Teriassic slate, phyllite, sandstone and Jurassic conglomerates crop out parallel to Sang bast- Shandize fault. Mineralization occurred as vein type, with trend of N65E to N50W with 75 degrees to t...

Journal: :پژوهش های جغرافیای طبیعی 0
الهه شفیعی سید احمد علوی نصیر نادری میقان

introduction tectonic of binaloud mountain ranges is controled by thrust faults system and folds related to these faults. parts of this mountain ranges and neyshabour plain is as study area in north eastern iran and between latitudes 36° 11´ 00 to 36° 30´ 00 and longitudes 58° 35´ 00 to 59° 00´ 00. in this paper we first study morphometric indices in this area then analyze drainages and allovia...

Journal: :رخساره های رسوبی 0
بهنام رحیمی فرزین قائمی

binaloud mountains formed during collision of iran and turan plate in the late triassic time and caused shortening of the sedimentary cover because of cimmerian and alpine orogeny. the thrust sheets with different generations formed as a results of the binalood and alborz fold- thrust belts. northeast of iran that was already south coast of the divergent margin of the paleothetys ocean at this ...

Journal: :Tectonics 2021

The timings of the onset oceanic spreading, subduction and collision are crucial in plate reconstructions, but not always straightforward to resolve. Paleo-Tethys evolution dominated Paleozoic-Early Mesozoic tectonics West Asia, timeline events is still poorly constrained. We present new detrital zircon ages from Binalud Mountains NE Iran, order determine timing tectonic region, wider implicati...

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