Ronit Kessel
Ronit Kessel
Institute of Earth Sciences, The Hebrew University of Jerusalem, Israel
Verified email at - Homepage
Cited by
Cited by
Trace element signature of subduction-zone fluids, melts and supercritical liquids at 120–180 km depth
R Kessel, MW Schmidt, P Ulmer, T Pettke
Nature 437 (7059), 724-727, 2005
The water–basalt system at 4 to 6 GPa: Phase relations and second critical endpoint in a K-free eclogite at 700 to 1400 C
R Kessel, P Ulmer, T Pettke, MW Schmidt, AB Thompson
Earth and Planetary Science Letters 237 (3-4), 873-892, 2005
A new model for the evolution of diamond-forming fluids: Evidence from microinclusion-bearing diamonds from Kankan, Guinea
Y Weiss, R Kessel, WL Griffin, I Kiflawi, O Klein-BenDavid, DR Bell, ...
Lithos 112, 660-674, 2009
Geomagnetic field intensity: How high can it get? How fast can it change? Constraints from Iron Age copper slag
R Shaar, E Ben-Yosef, H Ron, L Tauxe, A Agnon, R Kessel
Earth and Planetary Science Letters 301 (1-2), 297-306, 2011
Chromatographic metasomatism of the Arabian—Nubian lithosphere
M Stein, O Navon, R Kessel
Earth and Planetary Science Letters 152 (1-4), 75-91, 1997
The thermal history of equilibrated ordinary chondrites and the relationship between textural maturity and temperature
R Kessel, JR Beckett, EM Stolper
Geochimica et Cosmochimica Acta 71 (7), 1855-1881, 2007
Thermodynamic properties of the Pt-Fe system
R Kessel, JR Beckett, EM Stolper
American Mineralogist 86 (9), 1003-1014, 2001
Petrogenesis of Late Neoproterozoic dikes in the Northern Arabian–Nubian Shield: implications for the origin of A-type granites
R Kessel, M Stein, O Navon
Precambrian Research 92 (2), 195-213, 1998
A novel approach to determine high-pressure high-temperature fluid and melt compositions using diamond-trap experiments
R Kessel, P Ulmer, T Pettke, MW Schmidt, AB Thompson
American Mineralogist 89 (7), 1078-1086, 2004
Fluids in the peridotite–water system up to 6 GPa and 800 C: new experimental constrains on dehydration reactions
O Dvir, T Pettke, P Fumagalli, R Kessel
Contributions to Mineralogy and Petrology 161, 829-844, 2011
Testing the accuracy of absolute intensity estimates of the ancient geomagnetic field using copper slag material
R Shaar, H Ron, L Tauxe, R Kessel, A Agnon, E Ben-Yosef, JM Feinberg
Earth and Planetary Science Letters 290 (1-2), 201-213, 2010
Chromium mobility in hydrous fluids at upper mantle conditions
O Klein-BenDavid, T Pettke, R Kessel
Lithos 125 (1-2), 122-130, 2011
Melting of metasomatized peridotite at 4–6 GPa and up to 1200 C: an experimental approach
R Kessel, T Pettke, P Fumagalli
Contributions to Mineralogy and Petrology 169, 1-19, 2015
A new perspective on the interiors of ice-rich planets: ice–rock mixture instead of ice on top of rock
A Vazan, R Sari, R Kessel
The Astrophysical Journal 926 (2), 150, 2022
The effect of CO2 on the water-saturated solidus of K-poor peridotite between 4 and 6 GPa
O Dvir, R Kessel
Geochimica et Cosmochimica Acta 206, 184-200, 2017
Paleomagnetic field intensity derived from non-SD: Testing the Thellier IZZI technique on MD slag and a new bootstrap procedure
R Shaar, H Ron, L Tauxe, R Kessel, A Agnon
Earth and Planetary Science Letters 310 (3-4), 213-224, 2011
Melting of H2O and CO2-bearing eclogite at 4–6 GPa and 900–1200 C: implications for the generation of diamond-forming fluids
O Elazar, D Frost, O Navon, R Kessel
Geochimica et Cosmochimica Acta 255, 69-87, 2019
The petrogenesis of calc-alkaline granites from the Elat massif, Northern Arabian–Nubian shield
A Weissman, R Kessel, O Navon, M Stein
Precambrian Research 236, 252-264, 2013
The activity of chromite in multicomponent spinels: Implications for T‐fO2 conditions of equilibrated H chondrites
R Kessel, JR Beckett, GR Huss, EM Stolper
Meteoritics & Planetary Science 39 (8), 1287-1305, 2004
The behaviour of incompatible elements during hydrous melting of metasomatized peridotite at 4-6 GPa and 1000-1200 C
R Kessel, P Fumagalli, T Pettke
Lithos, 2015
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