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Slab detachment beneath eastern Anatolia: A possible cause for the formation of the North Anatolian fault

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TLDR
In this article, the authors discuss the possibility that the North Anatolian fault (NAF) results from the deep deformation of the slab beneath the Bitlis-Hellenic subduction zone.
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This article is published in Earth and Planetary Science Letters.The article was published on 2006-02-15. It has received 348 citations till now. The article focuses on the topics: Slab pull & Slab window.

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Citations
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Zagros orogeny: a subduction-dominated process

TL;DR: In this paper, the authors presented a synthetic view of the geodynamic evolution of the Zagros orogen within the frame of the Arabia-Eurasia collision, and provided lithospheric-scale reconstructions of the zagros Orogen from ~ 150 to 0 Ma across two SW-NE transects.
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Building the Zagros collisional orogen: Timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence

TL;DR: In this paper, the authors show that only 42% of the post-35 Ma convergence is partitioned by shortening within central Iran, and the current subduction dynamics can be explained by the original lateral difference in the buoyancy of the distal margin.
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Arc-magmatism and subduction history beneath the Zagros Mountains, Iran: A new report of adakites and geodynamic consequences

TL;DR: In this article, the authors focus on the key geodynamic constraints provided by the subduction-related magmatism of the upper plate, which shifted ~ 300 km inward from the SSMA to the UDMA at the end of the Mesozoic.
References
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Active tectonics of Mediterranean region

TL;DR: In this article, the authors examined more than 100 fault plane solutions for earthquakes within the Alpide belt between the Mid-Atlantic ridge and Eastern Iran and found that the deformation at present occurring is the result of small continental plates moving away from Eastern Turkey and Western Iran.
Journal ArticleDOI

Active Tectonics of the Mediterranean Region

TL;DR: In this paper, the authors examined more than 100 fault plane solutions for earthquakes within the Alpide belt between the Mid-Atlantic ridge and Eastern Iran and found that the deformation at present occurring is the result of small continental plates moving away from Eastern Turkey and Western Iran.
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Global Positioning System constraints on plate kinematics and dynamics in the eastern Mediterranean and Caucasus

TL;DR: In this article, the authors present and interpret GPS measurements of crustal motions for the period 1988-1997 at 189 sites extending east-west from the Caucasus mountains to the Adriatic Sea and north-south from the southern edge of the Eurasian plate to the northern edge of Africa.
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The hellenic arc and trench system: A key to the neotectonic evolution of the eastern mediterranean area

TL;DR: In this paper, the authors used the fault plane mechanisms of shallow earthquakes along the Hellenic arc and the extent of the intermediate seismic belt to make a quantitative estimate of the relative motion occurring between the Hellenians arc and adjacent sea floor.
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