Oroclinal bending, distributed thrust and strike-slip faulting, and the accommodation of Arabia-Eurasia convergence in NE Iran since the Oligocene

Geophysical Journal International

Volumn 181, Issue 3, 2010, Pages 1214-1246

  Hollingsworth, James ^a   Fattahi, Morteza ^b,c   Walker, Richard ^c   Talebian, Morteza ^d   Bahroudi, Abbas ^b   Bolourchi, Mohammad Javad ^d   Jackson, James ^e   Copley, Alex ^a  

^a CALIFORNIA INSTITUTE OF TECHNOLOGY   (United States)

^b UNIVERSITY OF TEHRAN   (Iran)

^c UNIVERSITY OF OXFORD   (United Kingdom)

^d GEOLOGICAL SURVEY OF IRAN   (Iran)

^e UNIVERSITY OF CAMBRIDGE   (United Kingdom)

Author keywords

Asia; Continental neotectonics; Geomorphology; Seismicity and tectonics; Tectonics and landscape evolution

Indexed keywords

ARABIAN PLATE; BENDING; CRUSTAL SHORTENING; CRUSTAL THICKENING; DEFORMATION MECHANISM; EURASIAN PLATE; FORELAND BASIN; GPS; LANDSCAPE EVOLUTION; NEOTECTONICS; OLIGOCENE; PLATE CONVERGENCE; SEISMICITY; STRIKE-SLIP FAULT; TECTONIC EVOLUTION; TECTONIC SETTING; THRUST FAULT; UPLIFT;

ELBURZ; IRAN; KOPET-DAGH BASIN; RAZAVI KHORASAN; SABZEVAR;

EID: 77954146579     PISSN: 0956540X     EISSN: 1365246X     Source Type: Journal    
DOI: 10.1111/j.1365-246X.2010.04591.x     Document Type: Article

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