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Sökning: WFRF:(Nilfouroushan Faramarz Senior Lecturer 1968 ) > An up-to-date crust...

An up-to-date crustal deformation map of Iran using integrated campaign-mode and permanent GPS velocities

Khorrami, Fatemeh (författare)
National Cartographic Center, Tehran, Iran
Vernant, Philippe (författare)
Géosciences Montpellier, CNRS/University Montpellier, Montpellier, France
Masson, Frederic (författare)
IPGS/EOST CNRS/University Strasbourg, Strasbourg Cedex, France
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Nilfouroushan, Faramarz, Senior Lecturer, 1968- (författare)
Högskolan i Gävle,Samhällsbyggnad,Lantmäteriet, Gävle, Sweden
Mousavi, Zahra (författare)
Department of Earth Sciences, Institute for Advanced Studies in Basic Sciences (IASBS), Zanjan, Iran
Nankali, Hamidreza (författare)
National Cartographic Center, Tehran, Iran
Saadat, Seyed Abdolreza (författare)
National Cartographic Center, Tehran, Iran
Walpersdorf, Andrea (författare)
University Grenoble Alpes, CNRS, IRD, IFSTTAR, ISTerre, Grenoble, France
Hosseini, Sedighe (författare)
National Cartographic Center, Tehran, Iran
Tavakoli, Parastoo (författare)
National Cartographic Center, Tehran, Iran
Aghamohammadi, Azade (författare)
National Cartographic Center, Tehran, Iran
Alijanzade, Mahnaz (författare)
National Cartographic Center, Tehran, Iran
visa färre...
 (creator_code:org_t)
2019-01-28
2019
Engelska.
Ingår i: Geophysical Journal International. - : Oxford University Press. - 0956-540X .- 1365-246X. ; 217:2, s. 832-843
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • We present the most extensive and up-to-date unified GPS velocity field for Iran. We processed the data collected during 10 years (2006–2015) from the Iranian Permanent GNSS Network (IPGN) and combined them with previously published velocity solutions from GPS survey measurements during 1997–2013. We analysed this velocity field using a continuum approach to compute a new strain rate map for this region and we designed a block model based on the main geological, morphological, and seismic structures. Comparison between both approaches suggests similar results and allow us to present the first comprehensive first order fault slip rate estimates for the whole of Iran. Our results confirm most of the results from previous geodetic studies. But we also show a trade-off between the coupling ratio of the Iranian Makran subduction interface and the kinematic of the faults north of the Makran in the Jazmurian depression. Indeed, although too scarce to accurately estimate a coupling ratio, we show that coupling higher than 0.4 on the plate interface down to a depth of 25 km will induce extension on the E-W faults in the Jazmurian region. However, the sites close to the shoreline suggest a low coupling ratio, hence the coupling on this plate interface is probably more complicated than previously described and the Iranian Makran subduction interface mechanical behaviour might be similar to that on the Hellenic subduction zone.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)

Nyckelord

GPS
Iran
Strain
deformation
Zagros
Makran
Hållbar stadsutveckling
Sustainable Urban Development

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