Biryol, C. Berk
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3

Relationship between observed upper mantle structures and r..:

Biryol, C. Berk ; Wagner, Lara S. ; Fischer, Karen M..
Journal of Geophysical Research: Solid Earth.  121 (2016)  5 - p. 3393-3414 , 2016
 
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4

Overriding plate, mantle wedge, slab, and subslab contribut..:

Long, Maureen D. ; Biryol, C. Berk ; Eakin, Caroline M....
Geochemistry, Geophysics, Geosystems.  17 (2016)  7 - p. 2556-2575 , 2016
 
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5

Imaging the Nazca slab and surrounding mantle to 700 km dep..:

, In: Geodynamics of a Cordilleran orogenic system / edited by Peter G.DeCelles (Department of Geosciences, University of Arizona, Tucson, Arizona, USA), Mihai N. Ducea (Department of Geosciences, University of Arizona, Tucson, Arizona, USA, and Universitatea Bucuresti, Facultatea de Geologie Geofizics Strada N. Balcescu Nr 1, Bucuresti, Romania) [und 2 weitere]
Scire, Alissa ; Biryol, C. Berk ; Zandt, George.. (2015)  - p. 23-41
Copies:  Zentrale:Magazin 02.k.2915
 
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9

Segmented African lithosphere beneath the Anatolian region ..:

Berk Biryol, C. ; Beck, Susan L. ; Zandt, George.
Geophysical Journal International.  184 (2011)  3 - p. 1037-1057 , 2011
 
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11

Detecting the limit of slab break-off in central Turkey: ne..:

Gans, Christine R. ; Beck, Susan L. ; Zandt, George..
Geophysical Journal International.  179 (2009)  3 - p. 1566-1572 , 2009
 
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13

Subduction termination through progressive slab deformation..:

Portner, Daniel Evan ; Delph, Jonathan R ; Biryol, C. Berk...
https://pubs.geoscienceworld.org/gsa/geosphere/article/14/3/907/530928/Subduction-termination-through-progressive-slab.  , 2018
 
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14

Subduction termination through progressive slab deformation..:

Portner, Daniel Evan ; Delph, Jonathan R ; Biryol, C. Berk...
Portner D. E. , Delph J. R. , Biryol C. B. , Beck S. L. , Zandt G., ÖZACAR A. A. , Sandvol E., TÜRKELLİ N., "Subduction termination through progressive slab deformation across Eastern Mediterranean subduction zones from updated P-wave tomography beneath Anatolia", GEOSPHERE, cilt.14, ss.907-925, 2018.  , 2018
 
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