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Kinematic variation...
Kinematic variation within the Fars Arc, eastern Zagros, and the development of fold‐and‐thrust belt curvature
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- Edey, A. (författare)
- University of Durham, UK
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- Allen, M. B (författare)
- University of Durham, UK
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- Nilfouroushan, Faramarz, Senior Lecturer, 1968- (författare)
- Högskolan i Gävle,Samhällsbyggnad,Lantmäteriet
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(creator_code:org_t)
- AGU, 2020
- 2020
- Engelska.
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Ingår i: Tectonics. - : AGU. - 0278-7407 .- 1944-9194. ; 39:8
- Relaterad länk:
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https://doi.org/10.1...
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https://hig.diva-por... (primary) (Raw object)
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https://urn.kb.se/re...
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https://doi.org/10.1...
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Abstract
Ämnesord
Stäng
- We analyze deformation of the Fars Arc in the eastern Zagros, Iran, including earthquake slip vectors, GPS velocities, paleomagnetism data, and fold orientations, to understand how this fold‐and‐thrust belt works, and so better understand the generic issue of fold‐and‐thrust belt curvature. The Fars Arc is curved, convex southwards. GPS‐derived rotation rates are ≤0.5° Myr‐1: rotation is clockwise west of 53° E, and counter‐clockwise to the east. These rotation senses are opposite to previous predictions of passive “bookshelf” models for strike‐slip faults during north‐south convergence. West of 53° E, average GPS vectors, thrust earthquake slip vectors, strain axes derived from GPS data and orthogonal directions to fold trends are all aligned, towards ~218°. East of this meridian, the average GPS vector is towards 208°, but the averages of the other datasets are distinctly different, all towards ~190°. We propose that fault blocks in eastern Fars, each ~20‐40 km long, rotate predominantly counter‐clockwise, whereas in western Fars the regional clockwise rotation takes place mainly on the array of active right‐lateral faults in this area. Thus localized block faulting and rotations accumulate to produce the overall strain and regional curvature. Active folds of different orientations in eastern Fars intersect to produce domal interference patterns, without involving separate deformation phases, indicating that fold interference patterns should not be interpreted in terms of changing stress orientations unless there is clear evidence. Fars Arc curvature is best explained by deformation being restricted at tectonic boundaries at its eastern and western margins, without significant gravitational spreading.
Ämnesord
- NATURVETENSKAP -- Geovetenskap och miljövetenskap (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences (hsv//eng)
Nyckelord
- Zagros
- Curvature
- Crustal deformation
- Tectonics
- fold-and-thrust
- Iran
Publikations- och innehållstyp
- ref (ämneskategori)
- art (ämneskategori)
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