Holland has made fundamental and enduring contributions to petrology.[12] He was the first to show that surface rocks had been buried to over 70 km.[12] He has worked to construct a self-consistent thermodynamic database which describes equilibria among the multi-component mineral phases important in rocks and with full propagation of errors.[12] This work, among the most highly cited in the geosciences, now underpins most petrological research.[12] Recent advances include the calculation of mineral assemblages and compositions as a function of composition, pressure and temperature and the thermodynamic modelling of silicatemelts, critical to tectonic interpretations of deeply buried rocks.[12]
^ abHolland, Timothy John Barrington (1977). Structural and metamorphic evolution of eclogites and associated rocks in the central Tauern region of the eastern Alps (DPhil thesis). University of Oxford. OCLC321017954. EThOSuk.bl.ethos.459466.
^ abcHolland, T. J. B.; Richardson, S. W. (1979). "Amphibole zonation in metabasites as a guide to the evolution of metamorphic conditions". Contributions to Mineralogy and Petrology. 70 (2): 143. Bibcode:1979CoMP...70..143H. doi:10.1007/BF00374442. S2CID129025852.
^Timothy Holland publications indexed by the Scopus bibliographic database. (subscription required)
^Holland, T. J. B.; Powell, R. (1990). "An enlarged and updated internally consistent thermodynamic dataset with uncertainties and correlations: The system K₂–Na₂O–CaO–MgO–MnO–FeO–Fe₂O₃–Al₂O₃–TiO₂–SiO₂–C–H₂–O₂". Journal of Metamorphic Geology. 8: 89. doi:10.1111/j.1525-1314.1990.tb00458.x.
^ abcdefAnon (2014). "Dr Timothy Holland FRS". royalsociety.org. London: Royal Society. Archived from the original on 2 May 2014. One or more of the preceding sentences incorporates text from the royalsociety.org website where: