Results 81 to 90 of about 635 (143)

Reptile fauna of the Khajeh protected area, with assessingits similarities with physiogeographical area of the Iranian Lizards

open access: yesتاکسونومی و بیوسیستماتیک, 2015
Natural habitats of the Iranian reptiles in many areas of the country are destroying due to several reasons. In such conditions the protected areas can act as the shelter sites for many organisms. Therefore it seems quite necessary that, under management
Masoud Yousefi   +4 more
doaj  

Modelling Neanderthals' dispersal routes from Caucasus towards east. [PDF]

open access: yesPLoS One, 2023
Ghasidian E   +4 more
europepmc   +1 more source

The Pistacietea verae: a new class of open, deciduous woodlands in Middle and Southwestern Asia [PDF]

open access: yes
oai:repository.derby.ac.uk:q71q1Aims: To analyse the syntaxonomy of open, deciduous woodlands at the southern margin of the steppe zone in the colline and montane belts of the Pamir-Alai, western Tian Shan and Iranian Mountains (Irano-Turanian region ...
Naqinezhad, A.   +4 more
core   +1 more source

Pore-type characterization of the Shurijeh formation in the Kopet-Dagh Basin, Northeastern Iran, using the integration of petrographic data, well logs, and production data

open access: yesJournal of Petroleum Exploration and Production Technology
The Early Cretaceous (Neocomian-Barremian) Formation of the Shurijeh is located in the northeast of Iran, east of the Caspian Sea and consists of predominantly red detrital clastic and carbonate facies extending into the Kopet-Dagh Basin.
Zahra Mashayekhi   +4 more
doaj   +1 more source

Local and regional P-wave spectral attenuation model for Iran. [PDF]

open access: yesGeophys J Int, 2021
Moradian Bajestani E   +2 more
europepmc   +1 more source

Comparing palynofacies and palaeoenvironment of Sarcheshmeh Formation in Joragh and Sheikh section (east and west of Kopeh-Dagh Basin)

open access: yesJournal of Stratigraphy and Sedimentology Researches, 2014
1-Introduction: Kopeh-Dagh sedimentary basin is located in NE of Iran and is mainly composed of Mesozoic and Cenozoic sedimentary rocks (35 30ˊ-38 15ˊ N, 54 00-61 31ˊE)(Afshar-Harb 1994).
Mohsen Allameh   +2 more
doaj  

SEISMOGENIC NODES DEFINED BY PATTERN RECOGNITION IN THE CENTRAL PART OF THE ALPINEHIMALAYAN BELT [PDF]

open access: yes, 2016
Information on the areas prone to the strongest earthquakes in a region is very important for knowledgeable seismic hazard and risk assessment. We consider the central part of the Alpine-Himalayan Belt (Caucasus–Kopet Dagh-Alburz) for the recognition of ...
Gorshkov, A., Novikova, O.
core   +1 more source

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