Inhaltsbereich
Publications
(Co) Author: Sobolev, S. V.
(since 2012) [ All ]
-
(2013 online first): Quantifying the thermo-mechanical impact of plume arrival on continental break-up.. Tectonophysics.
-
(2013): Why has the Nazca plate slowed since the Neogene?. Geology, 41, 1, 31-34.| EDOC: 18968 | 10.1130/G33497.1 |
-
(2012): Modeling suggests that oblique extension facilitates rifting and continental break-up. Journal of Geophysical Research, 117, B08402.
-
(2012): Thermomechanical model reconciles contradictory geophysical observations at the Dead Sea Basin. Geochemistry Geophysics Geosystems (G3), 13, Q04011.
-
(2012): Modeling evolution of the San Andreas Fault System in northern and central California.. Geochemistry Geophysics Geosystems (G3), 13, Q08016.
-
(2012): Constraining kinetics of metastable olivine in the Marianas slab from seismic observations and dynamic models. Tectonophysics, 526-529, 48-55.
TOP-
(2012): Results of geophysical studies across the Dead Sea Transform: The Arava/Araba Valley and the Dead Sea Basin. Israel Journal of Earth Sciences, 58, 3-4, 2009/2010, 147-161.
-
(2013): High resolution 2D numerical models from rift to break-up: Crustal hyper-extension, Margin asymmetry, Sequential faulting.. General Assembly European Geosciences Union (Vienna, Austria 2013).| EDOC: 20412 |
-
(2012): The Thermo-Mechanical Impact of Plume Arrival on Continental Break-Up. General Assembly European Geosciences Union (Vienna, Austria 2012).| EDOC: 19147 |
-
(2012): Why does the convergence rate between Nazca and South America decrease since the Neogene?. Geodynamics Workshop 2012 (Wandlitz, Germany 2012).| EDOC: 19727 |
-
(2012): Why does the convergence rate between Nazca and South America slow since the Neogene?. AGU 2012 Fall Meeting (San Francisco, USA 2012).| EDOC: 19701 |