Strike-slip faulting, rotation, and along-strike elongation in the Kopeh Dagh mountains, NE Iran
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 geologic...
Main Authors: | Hollingsworth, J, Jackson, J, Walker, R, Gheitanchi, MR, Bolourchi, M |
---|---|
Formato: | Journal article |
Idioma: | English |
Publicado em: |
2006
|
Registos relacionados
-
Slip-rate on the Main Köpetdag (Kopeh Dagh) strike-slip fault, Turkmenistan, and the active tectonics of the South Caspian
Por: Walker, R, et al.
Publicado em: (2021) -
Oroclinal bending, distributed thrust and strike-slip faulting, and the accommodation of Arabia-Eurasia convergence in NE Iran since the Oligocene
Por: Hollingsworth, J, et al.
Publicado em: (2010) -
Study of main planktonic foraminifera(Turonian-Santonian) in Kopeh-Dagh sedimentary environment, NE Iran
Por: Meysam Shafiee Ardestani, et al.
Publicado em: (2021-10-01) -
Determination of the stress field in the Kopeh Dagh and Eastern Iran regions
Por: Ghasem Ghorbani ROSTAM
Publicado em: (2022-04-01) -
Palynology and paleoecology of Sarcheshmeh and Sanganeh formations at Baghak section (east of Kopeh-Dagh)
Por: Mahjooneh Keshmiri, et al.
Publicado em: (2014-11-01)