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- Q2711902 subject Q13293997.
- Q2711902 subject Q8727730.
- Q2711902 abstract "The East Anatolian Fault is a major strike-slip fault zone in eastern Turkey. It forms the transform type tectonic boundary between the Anatolian Plate and the northward-moving Arabian Plate. The difference in the relative motions of the two plates is manifest in the left lateral motion along the fault. The East and North Anatolian faults together accommodate the westward motion of the Anatolian Plate as it is squeezed out by the ongoing collision with the Eurasian Plate.The East Anatolian Fault runs in a northeasterly direction, starting from the Maras Triple Junction at the northern end of the Dead Sea Transform, and ending at the Karliova Triple Junction where it meets the North Anatolian Fault.From 1939 to 1999 a series of earthquakes progressed westwards along the North Anatolian Fault. But since 2003 there have been a series on the East Anatolian Fault. These started with the 2003 Bingöl earthquake and include the 2010 Elâzığ earthquake.".
- Q2711902 thumbnail Anatolian_Plate.png?width=300.
- Q2711902 wikiPageExternalLink TECTONICS%20OF%20THE%20REGION.
- Q2711902 wikiPageWikiLink Q13293997.
- Q2711902 wikiPageWikiLink Q181971.
- Q2711902 wikiPageWikiLink Q188521.
- Q2711902 wikiPageWikiLink Q259207.
- Q2711902 wikiPageWikiLink Q3064504.
- Q2711902 wikiPageWikiLink Q3115877.
- Q2711902 wikiPageWikiLink Q331093.
- Q2711902 wikiPageWikiLink Q3506205.
- Q2711902 wikiPageWikiLink Q43.
- Q2711902 wikiPageWikiLink Q47089.
- Q2711902 wikiPageWikiLink Q664573.
- Q2711902 wikiPageWikiLink Q8727730.
- Q2711902 wikiPageWikiLink Q924948.
- Q2711902 comment "The East Anatolian Fault is a major strike-slip fault zone in eastern Turkey. It forms the transform type tectonic boundary between the Anatolian Plate and the northward-moving Arabian Plate. The difference in the relative motions of the two plates is manifest in the left lateral motion along the fault.".
- Q2711902 label "East Anatolian Fault".
- Q2711902 depiction Anatolian_Plate.png.