Results 11 to 20 of about 1,523 (113)
Short-term seismic crustal deformation of Iran [PDF]
In this paper the short-term seismic deformation of Iran is determined by the earthquake moment tensor summation. The study areas include the Alborz, Kopeh-Dagh, eastern Iran, Makran and Zagros orogenic belts.
Shoja Ansari, Ahmad Zamani
doaj +10 more sources
Palynostratigraphy of the Sanganeh Formation at the East and Central Kopeh-Dagh Basin based on dinoflagellate cysts [PDF]
The Sanganeh Formation (Lower Cretaceous) has cropped out across the Kopeh-Dagh Basin. The formation conformably overly the Aptian Sarcheshmeh Formation and is in turn overlain conformably by glauconitic sandstone of the Aitamir Formation. The considered
Narges Shokri +2 more
doaj +4 more sources
Comparing palynofacies and palaeoenvironment of Sarcheshmeh Formation in Joragh and Sheikh section (east and west of Kopeh-Dagh Basin) [PDF]
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 +3 more sources
Strike-slip faulting, rotation, and along-strike elongation in the Kopeh Dagh mountains, NE Iran [PDF]
SUMMARY The Kopeh Dagh is a linear mountain range separating the shortening in Iran from the stable, flat Turkmenistan platform. In its central part is an array of active right-lateral strike-slip faults that obliquely cut the range and produce offsets of several kilometres in the geomorphology and geological structure.
Hollingsworth, J +4 more
core +3 more sources
Quaternary slip rates along the northeastern boundary of the Arabia-Eurasia collision zone (Kopeh Dagh Mountains, Northeast Iran) [PDF]
P>The Kopeh Dagh is accommodating a large portion of the northward motion of central Iran with respect to Eurasia, involving a major right-lateral strike-slip fault system (Bakharden-Quchan). This fault system corresponds to the northeastern boundary of the Arabia-Eurasia collision, and can be considered as a lithospheric-scale tectonic feature.
Shabanian, Esmaeil +4 more
openaire +4 more sources
Kalateh Pialeh prospect area is located in the Kopeh Dagh zone, approximately 15 km northeastern of Esfarayen city. The area is composed of sedimentary rocks deposited during the Jurassic, Cretaceous, and Tertiary periods, which include microconglomerate,
Maryam Javidi Moghaddam +2 more
doaj +2 more sources
1-Introduction The Kopeh-Dagh as an inverted basin (Allen et al. 2003) is extended from the east of the Caspian Sea to NE Iran, north Afghanistan and Turkmenistan.
Mahjooneh Keshmiri +4 more
doaj +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 +2 more sources
This study shows that ichonology can be used to refine sequence stratigraphy as well as to interpret the depositional environment of the Kalat Formation (Upper Maastrichtian) in the Central Kopeh- Dagh Basin (NE Iran), Dareh-Gaz section. Field studies and petrography of these deposits led to recognize four lithofacies and nine subfacies that formed in ...
Torghabeh, A. +3 more
core +4 more sources
The Kopeh Dagh mountain belt is one of the most tectonically and seismically active regions in the central Eurasian collision zone, having experienced numerous moderate to large earthquakes (Mw ≥ 5.1) in recent decades. This study presents a novel structural and geodynamic analysis of ongoing deformation in the Kopeh Dagh Belt through the integration ...
Maryam Ezati +7 more
openaire +3 more sources

