| Subduction zone processes | Origin of lunar basalts | Mars magmatism and water on Mars |
| Magmatic processes on meteorite parent bodies | Archean komatiites | Planetary differentiation |
| Magmas from the lithosphere-asthenosphere boundary | Formation and stabilization of cratonic lithosphere |
| Mantle melting beneath mid-ocean ridges |


1. Parman, S.W., Kurz, M.D., Hart, S.R., Grove, T.L. (2005) Helium solubility in olivine and implications for high He-3/He-4 in ocean island basalts, Nature,437 ,1140-1143.

2. Holzheid, A., Grove, T.L. (2005) The effect of metal composition on Fe-Nipartition behavior between olivine and FeNi-metal, FeNi-carbide, FeNi-sulfide at elevated pressure. Chem. Geol. 221, 207-224.

3. Holzheid, A.H., Grove, T.L. (2003) Sulfur saturation limits in silicate meltsand their implications for core formation scenarios for terrestrial planets. Amer. Mineral. 87, 227-237.

4. A. Holzheid, M.D. Schmitz and T. L. Grove (2000) Textural equilibria of iron sulfide liquids in partly molten silicate aggregates andtheir relevance to core formation scenarios. J. Geophys. Res., 105, p. 13555 -13567.

5. K.T. Koga, N. Shimizu and T.L. Grove (1999) Disequilibrium trace element re-distribution during garnet to spinel facies transformation. In Proc. 7th Intl. Kimberlite Conf. J. J. Gurney et al., eds. , Red Roof design, Cape Town, p. 444 - 451.

6. T.L. Grove (1999) Origin of magmas. In Encyclopedia of Volcanoes, H. R. Sigurdsson, ed., Academic Press, p. 133 - 147.

7. G.A. Gaetani and T.L. Grove (1999) Wetting of mantle olivine by sulfide melt: Implications for Re/Os ratios in mantle peridotite and late - stage core formation. Earth Planet. Sci. Lett., 169, p. 147 - 163.

8. G.A. Gaetani and T.L. Grove (1997) Partitioning of moderately siderophile elements among olivine, silicate melt and sulfide melt: Constraints on core formation in Earth and Mars. Geochim. Cosmochim. Acta, 61, p. 1829 -1846.

9. H.-J. Yang, R.J. Kinzler and T.L. Grove (1996) Experimental constraints on the compositions of anhydrous olivine - plagioclase - augite saturated melts from 0.001 to 10 kbar in the natural system. Contrib. Mineral.Petrol., 124, p. 1 - 18.

10. G.A. Gaetani and T.L. Grove (1995) Partitioning of rare - earth elements between clinopyroxene and silicate melt: Crystal - chemical controls. Geochim. Cosmochim. Acta, 59, p. 1951 - 1962.

11. E.H. Hauri, T.P. Wagner and T.L. Grove (1994) Experimental and natural partitioning of Th, U, Pb and other trace elements between garnet, clinopyroxene and basaltic melts. Chem. Geol., 117, p. 149 - 166.