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An up-to-date block model and strain rate map of Iran using integrated campaign-mode and permanent GPS velocities
National Cartographic Center, Geodesy and Land Surveying, Tehran, Iran (Islamic Republic of).
Géosciences Montpellier- CNRS, Geosciences, Montpeliier, France.
IPGS/EOST CNRS/University Strasbourg, Earth Sciences, Strasbourg, France.
Högskolan i Gävle, Akademin för teknik och miljö, Avdelningen för datavetenskap och samhällsbyggnad, Samhällsbyggnad. Lantmäteriet, Gävle, Sweden.ORCID-id: 0000-0003-1744-7004
Vise andre og tillknytning
2019 (engelsk)Inngår i: 27th IUGG General Assembly: G06 - Posters - Monitoring and Understanding the Dynamic Earth With Geodetic Observations, 2019Konferansepaper, Poster (with or without abstract) (Fagfellevurdert)
Abstract [en]

Iran accommodates a large part of the ongoing Arabia-Eurasia collision deformation. Because of such active tectonics, the country suffers from intensive seismicity and frequent destructive earthquakes in different locations.To study further the crustal deformation in Iran, we processed the data collected during 10 years (2006-2015) from the Iranian Permanent GNSS Network 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. Moreover, 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. 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.

sted, utgiver, år, opplag, sider
2019.
Emneord [en]
GPS, deformation, Iran, strain, geodynamics
HSV kategori
Identifikatorer
URN: urn:nbn:se:hig:diva-29657OAI: oai:DiVA.org:hig-29657DiVA, id: diva2:1320151
Konferanse
27th IUGG General Assembly, 8-18 July, 2019, Montreal, Canada
Tilgjengelig fra: 2019-06-04 Laget: 2019-06-04 Sist oppdatert: 2019-08-08bibliografisk kontrollert

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