Results 31 to 40 of about 148 (98)
For the comparison of lithofacies in siliciclastic, carbonate, and mixed siliciclastic‐carbonate tidal systems, three successions including Top Quartzite (Lower‐Middle Cambrian), Deranjal Formation (Upper Cambrian), and Padeha Formation (Lower‐Middle Devonian) in the north of Kerman and Tabas regions (SE and E central Iran) were selected and described,
Hamed Zand-Moghadam +7 more
wiley +1 more source
In this paper, the biostratigraphy and sequence stratigraphy of marine Paleogene deposits from the Kopet‐Dagh basin (NE of Iran) are described. Particularly the absence of Morozovella genus is discussed. In addition, the Paleocene/Eocene boundary has been studied in detail using the record of planktonic and larger benthic foraminifera. This boundary is
Batool Rivandi +5 more
wiley +1 more source
Geology, petrology, geochemistry and geochronology of Tarik Darreh plutonic rocks, northeastern Iran
Introduction The investigated area in northeastern Iran that is known as the Tarik Darreh arsenopyrite-Au-W prospecting target is situated in the Kopeh Dagh zone (Fig. 1).
Jamal Ghavi +4 more
doaj +1 more source
Lg Coda Variations in North‐Central Iran
Ground motion records in north‐central Iran have been used in order to obtain the Lg coda Q, using stack spectral ratio method. The lateral variations in Q0 and its frequency dependence are estimated in the 0.3–7.0 Hz frequency range which led to Q = 267(±32) × f0.71(±0.14).
Mojtaba Naghavi +3 more
wiley +1 more source
Assessment of Climate Change Impacts on the Efficiency of Kopeh Dagh Conserved Area (Case study: Persian Gazella) [PDF]
Persian Gazelle (Gazella subgutturosa subgutturosa) is one of the most important herbivores of the steppes of Iran, which is found in different plains and desert areas. Today, the distribution of this species is limited to special areas, which has caused
Fateme Bagheri Azghadi +2 more
doaj +1 more source
Abstract The landscape of the Talesh Mountains, located in the NW sector of the Iranian Plateau (within the Arabia‐Eurasia collision zone), results from the interplay of multiple forces. To explore the interaction between tectonics, climate, and lithology we present 11 new erosion rates derived from meteoric 10Be on the eastern (wetter) and western ...
Mohammad Moumeni +8 more
wiley +1 more source
Major deserts do not necessarily consist of eolian dunes as quartz-rich as those of the Great Nafud, Rub’ al Khali, Sahara, and Mega-Kalahari sand seas accumulated in anorogenic settings of Arabia and Africa. The Karakum dune field of Turkmenistan is one
EDUARDO GARZANTI +3 more
doaj +1 more source
Block Rotations in NW Iran in Response to the Arabia‐Eurasia Collision Constrained by Paleomagnetism
Abstract Northwest Iran is a seismically active region dominated by NW‐SE trending strike‐slip faults, such as the North Tabriz and Qosha Dagh faults, and smaller NNE‐SSW striking faults. The Bozgush Mountains are shaped by these faults and divided into two domains that show a difference in strike. To quantify rotational tectonic deformation in NW Iran,
Ali Niknam +4 more
wiley +1 more source
Abstract The Kyzylkum Desert, as a transition area of different dust source in Central Asia, provides and reserves a large amount of dust transported by different atmospheric circulation systems, affecting Uzbekistan and downwind East Asia. However, there remains very few investigations about sediment sources and control factors of the desert.
Mingyu Zhang +5 more
wiley +1 more source
A comprehensive review of HVS‐I mitochondrial DNA variation of 19 Iranian populations
Abstract Iran is located along the Central Asian corridor, a natural artery that has served as a cross‐continental route since the first anatomically modern human populations migrated out of Africa. We compiled and reanalyzed the HVS‐I (hypervariable segment‐I) of 3840 mitochondrial DNA (mtDNA) sequences from 19 Iranian populations and from 26 groups ...
Motahareh Amjadi +4 more
wiley +1 more source

