| The deep carbon cycle and melting in Earth's interior R Dasgupta, MM Hirschmann Earth and Planetary Science Letters 298 (1-2), 1-13, 2010 | 1062 | 2010 |
| A possible role for garnet pyroxenite in the origin of the “garnet signature” in MORB MM Hirschmann, EM Stolper Contributions to Mineralogy and Petrology 124 (2), 185-208, 1996 | 932 | 1996 |
| Mantle solidus: Experimental constraints and the effects of peridotite composition MM Hirschmann Geochemistry, Geophysics, Geosystems 1 (10), 2000 | 906 | 2000 |
| The pMELTS: A revision of MELTS for improved calculation of phase relations and major element partitioning related to partial melting of the mantle to 3 GPa MS Ghiorso, MM Hirschmann, PW Reiners, VC Kress III Geochemistry, Geophysics, Geosystems 3 (5), 1-35, 2002 | 847 | 2002 |
| WATER, MELTING, AND THE DEEP EARTH H2O CYCLE MM Hirschmann Annu. Rev. Earth Planet. Sci. 34 (1), 629-653, 2006 | 697 | 2006 |
| Partial Melting Experiments of Peridotite + CO2 at 3 GPa and Genesis of Alkalic Ocean Island Basalts R Dasgupta, MM Hirschmann, ND Smith Journal of Petrology 48 (11), 2093-2124, 2007 | 672 | 2007 |
| Mg/Mn partitioning as a test for equilibrium between coexisting Fe-Ti oxides CR Bacon, MM Hirschmann American Mineralogist 73 (1-2), 57-61, 1988 | 653 | 1988 |
| Melting in the Earth's deep upper mantle caused by carbon dioxide R Dasgupta, MM Hirschmann Nature 440 (7084), 659-662, 2006 | 618 | 2006 |
| Alkalic magmas generated by partial melting of garnet pyroxenite MM Hirschmann, T Kogiso, MB Baker, EM Stolper Geology 31 (6), 481-484, 2003 | 610 | 2003 |
| Deep global cycling of carbon constrained by the solidus of anhydrous, carbonated eclogite under upper mantle conditions R Dasgupta, MM Hirschmann, AC Withers Earth and Planetary Science Letters 227 (1-2), 73-85, 2004 | 533 | 2004 |
| Compositions of near-solidus peridotite melts from experiments and thermodynamic calculations MB Baker, MM Hirschmann, MS Ghiorso, EM Stolper Nature 375 (6529), 308-311, 1995 | 527 | 1995 |
| High-pressure partial melting of garnet pyroxenite: possible mafic lithologies in the source of ocean island basalts T Kogiso, MM Hirschmann, DJ Frost Earth and Planetary Science Letters 216 (4), 603-617, 2003 | 499 | 2003 |
| Anhydrous partial melting experiments on MORB-like eclogite: phase relations, phase compositions and mineral–melt partitioning of major elements at 2–3 GPa M Pertermann, MM Hirschmann Journal of Petrology 44 (12), 2173-2201, 2003 | 489 | 2003 |
| Partial melting experiments on a MORB‐like pyroxenite between 2 and 3 GPa: Constraints on the presence of pyroxenite in basalt source regions from solidus location and melting rate M Pertermann, MM Hirschmann Journal of Geophysical Research: Solid Earth 108 (B2), 2003 | 415 | 2003 |
| Carbon-dioxide-rich silicate melt in the Earth’s upper mantle R Dasgupta, A Mallik, K Tsuno, AC Withers, G Hirth, MM Hirschmann Nature 493 (7431), 211-215, 2013 | 388 | 2013 |
| Hydrogen partition coefficients between nominally anhydrous minerals and basaltic melts C Aubaud, EH Hauri, MM Hirschmann Geophysical Research Letters 31 (20), 2004 | 372 | 2004 |
| Experimental determination of trace element partitioning between garnet and silica‐rich liquid during anhydrous partial melting of MORB‐like eclogite M Pertermann, MM Hirschmann, K Hametner, D Günther, MW Schmidt Geochemistry, Geophysics, Geosystems 5 (5), 2004 | 342 | 2004 |
| Dehydration melting of nominally anhydrous mantle: The primacy of partitioning MM Hirschmann, T Tenner, C Aubaud, AC Withers Physics of the Earth and Planetary Interiors 176 (1-2), 54-68, 2009 | 340 | 2009 |
| Immiscible Transition from Carbonate-rich to Silicate-rich Melts in the 3 GPa Melting Interval of Eclogite + CO2 and Genesis of Silica-undersaturated Ocean Island … R Dasgupta, MM Hirschmann, K Stalker Journal of Petrology 47 (4), 647-671, 2006 | 339 | 2006 |
| Storage capacity of H2O in nominally anhydrous minerals in the upper mantle MM Hirschmann, C Aubaud, AC Withers Earth and Planetary Science Letters 236 (1-2), 167-181, 2005 | 330 | 2005 |
