Sergio Zlotnik
Sergio Zlotnik
E-mail megerősítve itt:
Hivatkozott rá
Hivatkozott rá
Subduction dynamics and the origin of Andean orogeny and the Bolivian orocline
FA Capitanio, C Faccenna, S Zlotnik, DR Stegman
Nature 480 (7375), 83-86, 2011
Proper generalized decomposition for parameterized Helmholtz problems in heterogeneous and unbounded domains: Application to harbor agitation
D Modesto, S Zlotnik, A Huerta
Computer Methods in Applied Mechanics and Engineering 295, 127-149, 2015
The subductability of continental lithosphere: The before and after story
JC Afonso, S Zlotnik
Arc-Continent Collision, 53-86, 2011
Melt fracturing and healing: A mechanism for degassing and origin of silicic obsidian
A Cabrera, RF Weinberg, HMN Wright, S Zlotnik, RAF Cas
Geology 39 (1), 67-70, 2011
Proper generalized decomposition of a geometrically parametrized heat problem with geophysical applications
S Zlotnik, P Díez, D Modesto, A Huerta
International Journal for Numerical Methods in Engineering 103 (10), 737-758, 2015
Hierarchical X-FEM for n-phase flow (n> 2)
S Zlotnik, P Díez
Computer Methods in Applied Mechanics and Engineering 198 (30-32), 2329-2338, 2009
Effects of compositional and rheological stratifications on small‐scale convection under the oceans: Implications for the thickness of oceanic lithosphere and seafloor flattening
JC Afonso, S Zlotnik, M Fernandez
Geophysical Research Letters 35 (20), 2008
Numerical modelling of tectonic plates subduction using X-FEM
S Zlotnik, P Díez, M Fernández, J Vergés
Computer Methods in Applied Mechanics and Engineering 196 (41-44), 4283-4293, 2007
Small-scale gravitational instabilities under the oceans: Implications for the evolution of oceanic lithosphere and its expression in geophysical observables
S Zlotnik, JC Afonso, P Diez, M Fernández
Philosophical magazine 88 (28-29), 3197-3217, 2008
Generalized parametric solutions in Stokes flow
P Díez, S Zlotnik, A Huerta
Computer Methods in Applied Mechanics and Engineering 326, 223-240, 2017
Proper generalized decomposition solution of the parameterized Helmholtz problem: application to inverse geophysical problems
M Signorini, S Zlotnik, P Díez
International Journal for Numerical Methods in Engineering 109 (8), 1085-1102, 2017
An error estimator for real-time simulators based on model order reduction
I Alfaro, D González, S Zlotnik, P Díez, E Cueto, F Chinesta
Advanced Modeling and Simulation in Engineering Sciences 2 (1), 1-16, 2015
A stable extended FEM formulation for multi‐phase problems enforcing the accuracy of the fluxes through Lagrange multipliers
P Diez, R Cottereau, S Zlotnik
International journal for numerical methods in engineering 96 (5), 303-322, 2013
Algebraic PGD for tensor separation and compression: an algorithmic approach
P Díez, S Zlotnik, A García-González, A Huerta
Comptes Rendus Mécanique 346 (7), 501-514, 2018
Effect of the separated approximation of input data in the accuracy of the resulting PGD solution
S Zlotnik, P Díez, D Gonzalez, E Cueto, A Huerta
Advanced modeling and simulation in engineering sciences 2 (1), 1-14, 2015
Encapsulated PGD algebraic toolbox operating with high-dimensional data
P Diez, S Zlotnik, A Garcia-Gonzalez, A Huerta
Archives of computational methods in engineering 27 (4), 1321-1336, 2020
Numerical modelling of multiphase multicomponent reactive transport in the Earth’s interior
B Oliveira, JC Afonso, S Zlotnik, P Diez
Geophysical Journal International 212 (1), 345-388, 2018
Modelling gravitational instabilities: slab break-off and Rayleigh-Taylor diapirism
S Zlotnik, M Fernández, P Díez, J Vergés
Earth Sciences and Mathematics, 1491-1510, 2008
Controls on subduction reorganization in the Hellenic margin, eastern Mediterranean
FA Capitanio, S Zlotnik, C Faccenna
Geophysical research letters 37 (14), 2010
Solution of geometrically parametrised problems within a CAD environment via model order reduction
R Sevilla, S Zlotnik, A Huerta
Computer methods in applied mechanics and engineering 358, 112631, 2020
A rendszer jelenleg nem tudja elvégezni a műveletet. Próbálkozzon újra később.
Cikkek 1–20