Post-Collisional Tectonics and Magmatism in the Eastern Mediterranean Region

2006-01-01

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Quaternary mafic lavas in Central Anatolia provide geochemical insights into melt generation processes following regional delamination of the subducted Tethyan slabs. New geochemical data from the Pleistocene Hasandağ Cinder Cone Province (HCCP) and Karapınar Volcanic Field (KVF) record contributions from subduction-modified lithospheric and sub-lithospheric source domains that are distinct from those sampled elsewhere across Anatolia (e.g., Pearce et al., 1990; Aldanmaz et al., 2006; Keskin, 2007; Chakraba...
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The Central Pontides is an orogenic belt evolved since Triassic by the progressive closure of Paleo- and Neo-Tethys oceans, which is bounded by the IzmirAnkara-Erzincan Suture (Northern Neotethyan Suture) from the south. The post-Triassic Neo-Tethyan evolution in Amasya region started with Liassic transgression on the rifted pre-Liassic basement rocks. Later, the initial rifting failed and the platform was uplifted. The uplifted platform turned into an open-marine depositional realm as recorded by the depos...
Post delamination magmatism at the Hasandag Cinder cone province Central Anatolia
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Central Anatolian mafic lavas record both closure of the Tethyan Ocean and post-Miocene extension. Regional-scale delamination of the horizontally-subducted Neotethyan slab beneath Central Anatolia 9-14 Ma is inferred on the basis of >1 km of uplift of the Central Anatolian Plateau and the onset of widespread volcanism induced by melting of ascending asthenosphere (Bartol and Govers, 2014). Geochemical data from the Quaternary Hasandağ Cinder Cone Province suggest a more complicated story and require meltin...
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Central Anatolia, located on the immense Alpine-Himalayan orogenic belt, has a complicated neotectonic evolution, and NE-SW-trending Neogene horsts-graben systems that rejuvenate pre-existing palaeostructures are among the most important structures which help us understand the tectonic evolution of Central Anatolia.
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This thesis examines the migration patterns in Kyrgyzstan that have emerged after the independence period and the approach of Uzbek community in the country to migration and the preferable migration destinations within the framework of push and pull factors. Uzbeks, who are the second major ethnic group in Kyrgyzstan, live compactly in the southern provinces- Osh, Jalal-Abad, and Batken. They comprise one third of the region’s population and 14 percent of the country’s total population. In Kyrgyzstan, migra...
Citation Formats
N. T. Güleç, Post-Collisional Tectonics and Magmatism in the Eastern Mediterranean Region. 2006.