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- Nilforoushan, Faramarz, et al.
(författare)
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GPS network monitors the Arabia-Eurasia collision deformation in Iran
- 2003
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Ingår i: Journal of Geodesy. - : Springer Science and Business Media LLC. - 0949-7714 .- 1432-1394. ; 77, s. 411-422
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Tidskriftsartikel (refereegranskat)abstract
- The rate of crustal deformation in Iran due to the Arabia–Eurasia collision is estimated. The results are based on new global positioning system (GPS) data. In order to address the problem of the distribution of the deformation in Iran, Iranian and French research organizations have carried out the first large-scale GPS survey of Iran. A GPS network of 28 sites (25 in Iran, two in Oman and one in Uzbekistan) has been installed and surveyed twice, in September 1999 and October 2001. Each site has been surveyed for a minimum observation of 4 days. GPS data processing has been done using the GAMIT-GLOBK software package. The solution displays horizontal repeatabilities of about 1.2 mm in 1999 and 2001. The resulting velocities allow us to constrain the kinematics of the Iranian tectonic blocks. These velocities are given in ITRF2000 and also relative to Eurasia. This last kinematic model demonstrates that (1) the north–south shortening from Arabia to Eurasia is 2–2.5 cm/year, less than previously estimated, and (2) the transition from subduction (Makran) to collision (Zagros) is very sharp and governs the different styles of deformation observed in Iran. In the eastern part of Iran, most of the shortening is accommodated in the Gulf of Oman, while in the western part the shortening is more distributed from south to north. The large faults surrounding the Lut block accommodate most of the subduction–collision transition.
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| 2. |
- Tavakoli, Assad A, et al.
(författare)
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The effect of traffic flow improvements on driver attitudes towards pavement markings and other traffic control devices and pedestrian safety
- 2001
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Ingår i: Proceedings of the conference Traffic Safety on Three Continents. - Linköping : Statens väg- och transportforskningsinstitut. ; , s. 584-592
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Konferensbidrag (övrigt vetenskapligt/konstnärligt)abstract
- The author notes that many drivers today, especially those outside of major metropolitan areas, have not ever been pedestrians in the usual way. They may walk to their cars or through parking lots to mall entrances, but they rarely walk on public streets. Since they are not used to being pedestrians, many of them do not know how to behave towards pedestrians when they are behind the wheel of a car. In addition, some of the current traffic flow improvements provide the driver with more choices to make, sometimes leaving the pedestrian to the bottom choice. Right turn on red laws and arrows (and in some states left turn on red is permitted) frequently encourage the pedestrians to race for the curb in order to avoid being hit by the turning vehicle. Radios, cell phones, on board computers, and other amenities available in today's cars further distract the drivers from paying attention to pedestrian pavement markings and the pedestrians in them.
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| 3. |
- Vernant, P, et al.
(författare)
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Present-day crustal deformation and plate kinematics in the Middle East constrained by GPS measurements in Iran and northern Oman
- 2004
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Ingår i: Geophysical Journal International. - 0956-540X .- 1365-246X. ; 157:1, s. 381-398
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Tidskriftsartikel (refereegranskat)abstract
- A network of 27 GPS sites was implemented in Iran and northern Oman to measure displacements in this part of the Alpine–Himalayan mountain belt. We present and interpret the results of two surveys performed in 1999 September and 2001 October. GPS sites in Oman show northward motion of the Arabian Plate relative to Eurasia slower than the NUVEL-1A estimates (e.g. 22 ± 2 mm yr−1 at N8°± 5°E instead of 30.5 mm yr−1 at N6°E at Bahrain longitude). We define a GPS Arabia–Eurasia Euler vector of 27.9°± 0.5°N, 19.5°± 1.4°E, 0.41°± 0.1° Myr−1. The Arabia–Eurasia convergence is accommodated differently in eastern and western Iran. East of 58°E, most of the shortening is accommodated by the Makran subduction zone (19.5 ± 2 mm yr−1) and less by the Kopet-Dag (6.5 ± 2 mm yr−1). West of 58°E, the deformation is distributed in separate fold and thrust belts. At the longitude of Tehran, the Zagros and the Alborz mountain ranges accommodate 6.5 ± 2 mm yr−1 and 8 ± 2 mm yr−1 respectively. The right-lateral displacement along the Main Recent Fault in the northern Zagros is about 3 ± 2 mm yr−1, smaller than what was generally expected. By contrast, large right-lateral displacement takes place in northwestern Iran (up to 8 ± mm yr−1). The Central Iranian Block is characterized by coherent plate motion (internal deformation <2 mm yr−1). Sites east of 61°E show very low displacements relative to Eurasia. The kinematic contrast between eastern and western Iran is accommodated by strike-slip motions along the Lut Block. To the south, the transition zone between Zagros and Makran is under transpression with right-lateral displacements of 11 ± 2 mm yr−1.
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