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Non-parametric spatiotemporal trends in fire: An approach to identify fire regimes variations and predict seasonal effects of fire in Iran. [PDF]
Karami P, Tavakoli S.
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Phytotoxins Produced by <i>Diplodia</i> and Other Fungal Species Involved in Oak (<i>Quercus</i>) Diseases. [PDF]
Evidente A.
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Molecules, Morphometrics and Modeling of the Medically Important Genus <i>Hemiscorpius</i> Peters, 1861 (Scorpiones: Hemiscorpiidae) in Iran Reveal New Species from Kerman. [PDF]
Dehghan H +6 more
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The latest structures and seismicity of Zagros
Moscow University Bulletin. Series 4. Geology, 2022The modern structure of the Zagros folding-thrust structure was formed under the influence of collision processes on the eastern flank of the collision zone of Eurasia and Arabia. Based on structural-geomorphological analysis and spatio-temporal features of the seismicity distribution, the article considers the features of the latest and modern ...
N. V. Koronovskiy +4 more
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2020
The Zagros is the largest mountain range of the Iranian Plateau stretching from northeast Iraq to south Iran. It has high mountain peaks reaching the subnival zone in different parts though mostly in the central and southern Zagros. The climate is continental and the precipitation regime is Mediterranean with cold and wet winters and warm and dry ...
Noroozi, Jalil +3 more
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The Zagros is the largest mountain range of the Iranian Plateau stretching from northeast Iraq to south Iran. It has high mountain peaks reaching the subnival zone in different parts though mostly in the central and southern Zagros. The climate is continental and the precipitation regime is Mediterranean with cold and wet winters and warm and dry ...
Noroozi, Jalil +3 more
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THE PRE-ZAGROS INTEGRITY OF THE IRANIAN PLATFORM
Journal of Petroleum Geology, 1985The Hormoz Formation of InfraCambrian age is the oldest unit recognized in southern Iran. It consists mainly of salt, other evaporites and débris of basement rocks. Some huge blocks of the uppermost PreCambrian and Lower Cambrian layered rocks were lifted to the surface by uprising Hormoz salt.A detailed field investigation within three major salt ...
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THE ORIGIN OF THE ZAGROS DEFILES
1968While the westward-flowing streams of the Zagros mountains provide some of the world's most impressive canyon scenery, they also present an extremely perplexing problem of drainage genesis. Seldom are drainage anomalies as pronounced as they are among the great petrified waves of the Zagros.
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The kinematics of the Zagros Mountains (Iran)
Geological Society, London, Special Publications, 2010Abstract We present a synthesis of recently conducted tectonic, global positioning system (GPS), geomorphological and seismic studies to describe the kinematics of the Zagros mountain belt, with a special focus on the transverse right-lateral strike-slip Kazerun Fault System (KFS).
Hatzfeld, Denis +9 more
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2010
A Consular Officer in Bushire, serving in Mesopotamia and Luristan during First World War, Edmonds was sent to Qazvin after the war. He witnessed the Jangal upheaval and the 1921 coup d’Etat. The encounter with Persia of a well-trained and brilliant British agent.
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A Consular Officer in Bushire, serving in Mesopotamia and Luristan during First World War, Edmonds was sent to Qazvin after the war. He witnessed the Jangal upheaval and the 1921 coup d’Etat. The encounter with Persia of a well-trained and brilliant British agent.
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Holocene serial folding in the Zagros
Geological Society, London, Special Publications, 1988Abstract In the south-east Zagros Mountains of Iran, deformation during the Quaternary has occurred by serial folding, with the mountain front advancing westwards at 17 mm/yr. Coastal uplift during the Holocene indicates a horizontal slip of about 30 mm/yr.
C. D. Mann, C. Vita-Finzi
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