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 | 1388 | 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 | 349 | 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 | 211 | 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 | 140 | 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 | 104 | 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 | 98 | 2007 |
Thermodynamic properties of the Pt-Fe system R Kessel, JR Beckett, EM Stolper American Mineralogist 86 (9), 1003-1014, 2001 | 89 | 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 | 89 | 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 | 76 | 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 | 71 | 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 | 55 | 2010 |
Chromium mobility in hydrous fluids at upper mantle conditions O Klein-BenDavid, T Pettke, R Kessel Lithos 125 (1-2), 122-130, 2011 | 53 | 2011 |
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 | 48 | 2022 |
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 | 43 | 2015 |
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 | 40 | 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 | 36 | 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 | 27 | 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 | 18 | 2013 |
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 | 14 | 2015 |
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 | 14 | 2004 |