Computer Science
Scientist
Institute of Earth Sciences, Hebrew University, Givat Ram, Jerusalem 91904, Israel
The Hebrew University, Jerusalem, Israel
The Hebrew University of Jerusalem, Institute of Earth Sciences, Edmond Safra Campus, Givat-Ram, Jerusalem 91904, Israel
The Institute of Earth Sciences, The Hebrew University, Jerusalem, Israel
Institute of Earth Sciences, Hebrew University of Jerusalem, Jerusalem 91904, Israel. of Earth Sciences, The Hebrew University of Jerusalem, Givat Ram, 91904 Jerusalem, Israel
The Institute of Earth Sciences, The Hebrew University of Jerusalem, Givat Ram, Jerusalem, 91904, Israel
Institute of Earth Sciences, The Hebrew University of Jerusalem, Israel
Institute of Earth Sciences, Hebrew University of Jerusalem, 91904, Jerusalem, Israel
The Institute of Earth Sciences, The Hebrew University of Jerusalem, Givat Ram, Jerusalem 91904, Israel
Institute of Earth Sciences, Hebrew University, Jerusalem, 91904, Israel
California, University, Berkeley
Institute of Earth Sciences, Hebrew University, Jerusalem 91904, Israel
Institute of Earth Sciences, The Hebrew University, Jerusalem, Israel
Institute of Earth Sciences, Hebrew University of Jerusalem, 91904, Jerusalem, Israel. of Earth Sciences, The Hebrew University of Jerusalem, Givat Ram, Jerusalem, Israel
Institute of Earth Sciences, The Hebrew University of Jerusalem, 91904, Israel
Institute of Earth Sciences, The Hebrew University, Givat Ram, Jerusalem 91904, Israel.
A viscoelastic damage rheology and rate- and state-dependent friction
Calcitification of the last interglacial coral reefs in the Gulf of Aqaba - phreatic freshwater activity in the currently hyperarid region
Corrigendum to “Landscape development in an hyperarid sandstone environment along the margins of the Dead Sea fault: Implications from dated rock falls” [Earth Planet. Sci. Lett. 240 (2005) 803 817]
Coupled evolution of damage and porosity in poroelastic media: theory and applications to deformation of porous rocks
Direct evidence for dynamic magma supply fossilized in the lower oceanic crust of the Troodos ophiolite
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