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The effects of subduction termination on the continental lithosphere: Linking volcanism, deformation, surface uplift, and slab tearing in central Anatolia
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Date
2017-11-01
Author
Delph, Jonathan R.
Abgarmi, Bizhan
Ward, Kevin M.
Beck, Susan L.
Özacar, Atilla Arda
Zandt, George
Sandvol, Eric
TÜRKELLİ, NİYAZİ
Kalafat, Dogan
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Subduction beneath central Anatolia represents the transition between continuous subduction along the Aegean trench in the west and slab break-off and/or subduction termination at the Arabian-Eurasian collision zone in the east. Using recently collected seismic data from the Continental Dynamics-Central Anatolian Tectonics project alongside a newly developed approach to the creation of a 3D shear-velocity model from the joint inversion of receiver functions and surface-wave dispersion data, we can gain important insights into the character of the downgoing, segmenting African lithosphere and its relationship with the overriding Central Anatolian plate.
Subject Keywords
Stratigraphy
,
Geology
URI
https://hdl.handle.net/11511/43896
Journal
GEOSPHERE
DOI
https://doi.org/10.1130/ges01478.1
Collections
Department of Geological Engineering, Article
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J. R. Delph et al., “The effects of subduction termination on the continental lithosphere: Linking volcanism, deformation, surface uplift, and slab tearing in central Anatolia,”
GEOSPHERE
, pp. 1788–1805, 2017, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/43896.