Thrust tectonics of the Binalood Region, NE Iran

作者: Mehdi Alavi

DOI: 10.1029/91TC02217

关键词: Thrust faultGeologyPaleontologyTectonicsThrust tectonicsStack (geology)Foreland basinGeomorphologyCretaceousPaleozoicCenozoicGeochemistry and PetrologyGeophysics

摘要: The Binalood region in NE Iran, which is an eastern segment of the Alborz Mountains, affected by thin-skinned tectonics. Lower Paleozoic, Jurassic, Cretaceous, and Cenozoic rock sequences as well remnants Paleo-Tethys oceanic realm are transported a southwestward direction several thrust faults two generations: (1) Cimmerian (2) Alpine. Structural units this form either single sheets or duplexes. They have been displaced sequentially piggyback style from hinterland (NE) to foreland (SW) under ductile, brittle-ductile, brittle conditions. Geometrically, they constitute antiformal stack breached on its southwestern side major minor out-of-sequence thrusts.

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