Ewald summation for systems with slab geometry

1999 ◽  
Vol 111 (7) ◽  
pp. 3155-3162 ◽  
Author(s):  
In-Chul Yeh ◽  
Max L. Berkowitz
Keyword(s):  
Ewald Summation ◽  
Slab Geometry

Modified 3D Ewald Summation for Slab Geometry at Constant Potential

2020 ◽  
Vol 124 (36) ◽  
pp. 7842-7848
Author(s):  
Matheus Girotto ◽  
Adriano Mesquita Alencar
Keyword(s):  
Ewald Summation ◽  
Slab Geometry ◽  
Constant Potential

scholarly journals Simulations of Coulomb systems with slab geometry using an efficient 3D Ewald summation method

2016 ◽  
Vol 144 (14) ◽  
pp. 144103 ◽  
Author(s):  
Alexandre P. dos Santos ◽  
Matheus Girotto ◽  
Yan Levin
Keyword(s):  
Coulomb Systems ◽  
Summation Method ◽  
Ewald Summation ◽  
Slab Geometry

scholarly journals Post-collisional mantle delamination in the Dinarides implied from staircases of Oligo-Miocene uplifted marine terraces

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Philipp Balling ◽  
Christoph Grützner ◽  
Bruno Tomljenović ◽  
Wim Spakman ◽  
Kamil Ustaszewski
Keyword(s):  
Balkan Peninsula ◽  
Receiver Functions ◽  
P Wave ◽  
S Wave ◽  
Slab Geometry ◽  
Surface Uplift ◽  
River Incision ◽  
Marine Terraces ◽  
Convergence System ◽  
Internal Dinarides

AbstractThe Dinarides fold-thrust belt on the Balkan Peninsula resulted from convergence between the Adriatic and Eurasian plates since Mid-Jurassic times. Under the Dinarides, S-wave receiver functions, P-wave tomographic models, and shear-wave splitting data show anomalously thin lithosphere overlying a short down-flexed slab geometry. This geometry suggests a delamination of Adriatic lithosphere. Here, we link the evolution of this continental convergence system to hitherto unreported sets of extensively uplifted Oligocene–Miocene (28–17 Ma) marine terraces preserved at elevations of up to 600 m along the Dinaric coastal range. River incision on either side of the Mediterranean-Black Sea drainage divide is comparable to the amounts of terrace uplift. The preservation of the uplifted terraces implies that the most External Dinarides did not experience substantial deformation other than surface uplift in the Neogene. These observations and the contemporaneous emplacement of igneous rocks (33–22 Ma) in the internal Dinarides suggest that the Oligo-Miocene orogen-wide uplift was driven by post-break-off delamination of the Adriatic lithospheric mantle, this was followed by isostatic readjustment of the remaining crust. Our study details how lithospheric delamination exerts an important control on crustal deformation and that its crustal signature and geomorphic imprint can be preserved for millions of years.

scholarly journals Seismicity and shallow slab geometry in the central Vanuatu subduction zone

2015 ◽  
Vol 120 (8) ◽  
pp. 5606-5623 ◽  
Author(s):  
Christian Baillard ◽  
Wayne C. Crawford ◽  
Valérie Ballu ◽  
Marc Régnier ◽  
Bernard Pelletier ◽  
...  
Keyword(s):  
Subduction Zone ◽  
Slab Geometry
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